31 July 2003
Usage note: CAPITALIZATION within a definition indicates that the term is defined elsewhere in the glossary. Figure numbers refer to the main text of the Coastal Engineering Manual.
The mechanical wearing away by rock material transported by wind or water
A rock or clay platform which has been worn by the processes of abrasion.
A device used in wave buoys for measuring acceleration.
May be either natural or artificial. Natural accretion is the buildup of land, solely by the action of the forces of
nature, on a beach by deposition of water- or airborne material. Artificial accretion is a similar buildup of land by reason of
an act of man, such as the accretion formed by a GROIN, BREAKWATER, or beach fill deposited by mechanical means.
A margin of a continental plate consisting of a continental shelf and slope, and an oceanic trench or basin.
A GROIN whose permeability can be changed, usually with gates or removable sections.
ADVANCE (of a beach)
(1) A continuing seaward movement of the shoreline. (2) A net seaward movement of the shoreline over a specified time. Also PROGRESSION.
Changes in a sea water property (salinity, temperature, oxygen content, etc.) that take place in the presence of
currents. Also, changes in atmospheric properties in the earth’s atmosphere.
The ratio of wave velocity to wind velocity (in wave forecasting theory).
The course along which the center line of a channel, canal or drain is located.
Detrital material which is transported by a river and deposited – usually temporarily – at points along the flood plain of a river. Commonly composed of sands and gravels.
A plain bordering a river, formed by the deposition of material eroded from areas of higher elevation.
Soil (sand, mud, or similar detrital material) deposited by streams, or the deposits formed.
Parallel to and near the shoreline; LONGSHORE.
An instrument that determines its distance above a particular surface.
An instrument that determines altitude by measuring the length of time needed for a pulse of coherent light to travel from the instrument to the surface and back, and multiplies half this time by the speed of light to get the straight-line distance to the surface.
See ALTIMETER, LASER.
(1) The magnitude of the displacement of a wave from a mean value. An ocean wave has an amplitude equal to the vertical distance from still-water level to wave crest. For a sinusoidal wave, the amplitude is one-half the wave height. (2) The semirange of a constituent tide.
Spongy underwater ice formed on a submerged object or attached to the bottom of a shallow body of water which is itself not frozen; syn. bottom ice
ANGLE OF REPOSE
The maximum slope (measured from the horizontal) at which soils and loose materials on the banks of canals, rivers or embankments will stay stable.
Having properties that change with changing directions.
Refers to an environment that contain little or no dissolved oxygen and hence little or no benthic marine life. These conditions arise in some basins or fjords where physical circulation of seawater is limited.
BED FORMS that occur in trains and are in phase with, and strongly interact with, gravity water-surface waves.
Layer of stone, concrete or other material to protect the toe of a structure.
AQUATIC MATERIAL PLACEMENT
Comprises all placement options under which the dredged material is submerged under water and remains
water-saturated after placement terminates.
A geologic formation that is water-bearing, and which transmits water from one point in the formation to another.
A sea that contains numerous islands; also the island group itself.
Protective layer on a BREAKWATER or SEAWALL composed of armor units.
ARMOR UNIT or STONE
A relatively large quarrystone or concrete shape that is selected to fit specified geometric characteristics and density. It is usually of nearly uniform size and usually large enough to require individual placement. In normal cases it is used as primary wave protection and is placed in thicknesses of at least two units.
The process of replenishing a beach with material (usually sand) obtained from another location.
The tidal levels and character which would result from gravitational effects, e.g. of the Earth, Sun and Moon, without any atmospheric influences.
A ring-shaped coral REEF, often carrying low sand islands, enclosing a shallow LAGOON. The reef is surrounded by deep water of the open sea.
(1) A lessening of the amplitude of a wave with distance from the origin. (2) The decrease of water-particle motion with increasing depth. Particle motion resulting from surface oscillatory waves attenuates rapidly with depth, and practically disappears at a depth equal to a surface wavelength.
A term applied to shelves on which older shelf sediments are primarily being reworked by modern shelf processes.
AUTOMATIC TIDE GAGE
An instrument that automatically registers the rise and fall of the tide. In some instruments, the registration is accomplished by printing the heights at regular intervals, in others by a continuous graph in which the height of the tide is represented by the ordinates of the curve and the corresponding time by the abscissae.
(1) Rapid EROSION of the shore land by waves during a storm. (2) A sudden cutting off of land by flood, currents or change in course of a body of water.
Situated so that the top is intermittently washed by waves or tidal action. Condition of being exposed or just bare at any stage of the tide between high water and chart datum.
Pertaining to the lagoon-marsh-tidal creek complex in the lee of a coastal barrier island, barrier spit, or baymouth barrier.
The seaward return of the water following the uprush of the waves. For any given tide stage the point of farthest
return seaward of the backrush is known as the Limit of backrush or limit backwash.
That zone of the shore or beach lying between the foreshore and the coastline comprising the BERM or BERMS
and acted upon by waves only during severe storms, especially when combined with exceptionally high water. Also
BACKBEACH. (See Figure A-1)
(1) See BACKRUSH. (2) Water or waves thrown back by an obstruction such as a ship, BREAKWATER, or cliff.
Low amplitude ripple marks formed on fine sand beaches by the Backwash of the waves.
The longitudinal profile of the water surface in an open channel where the depth of flow has been increased by an obstruction as a weir or a dam across the channel, by increase in channel roughness, by decrease in channel width or by a decrease of the bed gradient
(1) The rising ground bordering a lake, river, or sea; or of a river or channel, for which it is designated as right or left as the observer is facing downstream. (2) An elevation of the sea floor or large area, located on a continental (or island) shelf and over which the depth is relatively shallow but sufficient for safe surface navigation (e.g., Georges Bank); a group of shoals. (3) In its secondary sense, used only with a qualifying word such as “sandbank,” “gravelbank,” or “spoil bank,” a shallow area consisting of shifting forms of silt, sand, mud, and gravel.
A submerged or emerged embankment of sand, gravel, or other unconsolidated material built on the sea floor in
shallow water by waves and currents. See BAYMOUTH BAR, CUSPATE BAR.
A bar essentially parallel to the shore, the crest of which is above normal high water level. Also called offshore
barrier and BARRIER ISLAND.
The flat area, often marshy and populated with low vegetation, on the bay or lagoon side of a barrier island
|Definition of terms and features describing the coastal zone.|
A detached portion of a barrier beach between two inlets. It commonly has DUNES, vegetated areas, and swampy terranes (see BARRIER FLAT) extending from the beach into the lagoon. Example: Outer Banks, North Carolina.
A bay roughly parallel to the coast and separated from the open ocean by barrier islands. Also, the body of water encircled by coral islands and REEFS, in which case it may be called an ATOLL lagoon.
A coral REEF parallel to and separated from the coast by a lagoon that is too deep for coral growth. Generally, barrier reefs follow the coasts for long distances and are cut through at irregular intervals by channels or passes. Example: Great Barrier Reef, Queensland, Australia.
Similar to a BARRIER ISLAND, but connected to the mainland.
A depressed area with no surface outlet, such as a lake basin or an enclosed sea.
A naturally or artificially enclosed or nearly enclosed harbor area for small craft.
A massive groin, or projecting section of seawall normally constructed with its crest above water level.
A topographic map of the bed of the ocean, with depths indicated by contours (isobaths) drawn at regular intervals.
The measurement of water depths in oceans, seas, and lakes; also information derived from such measurements.
A recess in the shore or an inlet of a sea between two capes or headlands, not as large as a gulf but larger than a
cove. See also BIGHT, EMBAYMENT.
A bar extending partly or entirely across the mouth of a bay .
A minor sluggish waterway or estuarial creek, tributary to, or connecting, other streams or bodies of water, whose course is usually through lowlands or swamps. Sometimes called SLOUGH. Term is commonly used in the southern United States.
The zone of unconsolidated material that extends landward from the low water line to the place where there is marked change in material or physiographic form, or to the line of permanent vegetation (usually the effective limit of storm waves). The seaward limit of a beach--unless otherwise specified--is the mean low water line. A beach includes foreshore and backshore. (See Figure A-1) See also SHORE, SUSTAINABLE BEACH, and SELF-SUSTAINING BEACH, and TIDELANDS.
A nearly horizontal part of the beach or backshore formed by the deposit of material by wave action. Some beaches have no berms, others have one or several. (See Figure A-1)
The point representing the limit of normal HIGH TIDE wave run-up (see BERM CREST)
The carrying away of beach materials by wave action, tidal currents, littoral currents, or wind.
The section of the beach normally exposed to the action of the wave uprush. The FORESHORE of a BEACH. (Not synonymous with SHOREFACE.)
Material placed on a beach to renourish eroding shores, usually pumped by dredge but sometimes delivered by trucks.
The cliff, dune or sea wall looming above the land ward limit of the active beach
Granular sediments, usually sand or shingle moved by the sea.
See BEACH FILL.
BEACH PLAN SHAPE
The shape of the beach in plan; usually shown as a contour line, combination of contour lines or recognizable features such as beach crest and/or the still water line
A cross-section taken perpendicular to a given beach contour; the profile may include the face of a dune or sea wall, extend over the backshore, across the foreshore, and seaward underwater into the NEARSHORE zone.
See RIDGE, BEACH.
See SCARP, BEACH. BEACH WIDTH
The horizontal dimension of the beach measured normal to the shoreline and landward of the higher-high tide line (on oceanic coasts) or from the still water level (on lake coasts)
Classification of the force of the winds in accordance with a scale established by Rear-Admiral, Sir Francis Beaufort in which the range of intensity varies in integers from 0 to 12, with a description of the state and behavior of a "wellconditioned man-of-war."
|Table A-1 Beaufort Wind Scale |
|Beaufort Number ||Wind Speed (knots) ||WMO Description 1 |
|0 ||< 1 ||Calm |
|1 ||1 - 3 ||Light air |
|2 ||4 - 6 ||Light breeze |
|3 ||7 - 10 ||Gentle breeze |
|4 ||11 - 16 ||Moderate breeze |
|5 ||17 - 21 ||Fresh breeze |
|6 ||22 - 27 ||Strong breeze |
|7 ||28 - 33 ||Near gale |
|8 ||34 - 40 ||Gale |
|9 ||41 - 47 ||Strong Gale |
|10 ||48 - 55 ||Storm |
|11 ||56 - 63 ||Violent storm |
|12 ||$ 64 ||Hurricane |
The bottom of a watercourse, or any body of water.
Any deviation from a flat bed that is readily detectable by eye and higher than the largest sediment size present in the parent bed material; generated on the bed of an alluvial channel by the flow.
Sediment transport mode in which individual particles either roll or slide along the bed as a shallow, mobile layer a few particle diameters deep, the part of the load that is not continuously in suspension.
A (rock) structure on the bed in order to protect the underlying bed against erosion due to current and/or wave action.
BED SHEAR STRESS
The way in which waves (or currents) transfer energy to the sea bed.
A surface parallel to the surface of deposition, which may or may not have a physical expression. The original attitude of a bedding plane should not be assumed to have been horizontal.
The solid rock that underlies gravel, soil, and other superficial material. Bedrock may be exposed at the surface (an outcrop) or it may br buried under a few centimeters to thousands of meters of unconsolidated material.
(1) A level or gently sloping erosion plane inclined seaward. (2) A nearly horizontal area at about the level of maximum high water on the sea side of a dike.
BENCH MARK, TIDAL
A bench mark whose elevation has been determined with respect to MEAN SEA LEVEL at a nearby tide GAUGE; the tidal bench mark is used as reference for that tide gauge.
A permanently fixed point of known elevation. A primary bench mark is one close to a tide station to which the tide staff and tidal datum originally are referenced.
BENEFICIAL USE OF DREDGED MATERIAL
Placement or use of dredged material for some productive purpose. Examples: BEACH FILL or NEARSHORE BERM construction.
The asset value of a scheme, usually measured in terms of the cost of damages avoided by the scheme, or the valuation of perceived amenity or environmental improvements
Pertaining to the sub-aquatic bottom.
Those animals who live on the sediments of the sea floor, including both mobile and non-mobile forms.
(1) On a beach: a nearly horizontal plateau on the beach face or backshore, formed by the deposition of beach material by wave action or by means of a mechanical plant as part of a beach renourishment scheme. Some natural beaches have no berm, others have several. (2) On a structure: a nearly horizontal area, often built to support or key-in an armor layer.
See BEACH BERM.
Rubble mound structure with horizontal berm of armor stones at about sea level, which is allowed to be (re)shaped by the waves.
The seaward limit of a BERM. Also called BERM EDGE. (See Figure A-1)
A bend in a coastline forming an open BAY. A BAY formed by such a bend.
The disturbance of sediment bedding by the activities of burrowing organisms.
A river DELTA formed by many levee-bordered DISTRIBUTARIES extending seaward and resembling in plan the outstretched claws of a bird. Example: Mississippi River delta.
BLANKET (FOUNDATION or BEDDING)
A layer or layers of graded fine stones underlying a BREAKWATER, GROIN or rock embankment to prevent the natural bed material from being washed away.
See EOLIAN SANDS.
A depression on the land surface caused by wind erosion.
A high, steep bank or cliff.
A wet, spongy, poorly drained area which is usually rich in very specialized plants, contains a high percentage of organic remnants and residues and frequently is associated with a spring, seepage area, or other subsurface water source. A bog sometimes represents the final stage of the natural processes of eutrophication by which lakes and other bodies of water are very slowly transformed into land areas.
An upward flow of water in a sandy formation due to an unbalanced hydrostatic pressure resulting from a rise in a nearby stream, or from removing the overburden in making excavations.
A prominent landmass that rises steeply from the sea.
A very rapid rise of the tide in which the advancing water presents an abrupt front of considerable height. In shallow estuaries where the range of tide is large, the high water is propagated inward faster than the low water because of the greater depth at high water. If the high water overtakes the low water, an abrupt front is presented, with the high-water crest finally falling forward as the tide continues to advance. Also EAGER.
BOTTOM (nature of)
The composition or character of the bed of an ocean or other body of water (e.g., clay, coral, gravel, mud, ooze,
pebbles, rock, shell, shingle, hard, or soft). (See Figure A-1)
BOTTOM BOUNDARY LAYER
The lower portion of the water flow that experiences frictional retardation based on its proximity to the bed.
One of the horizontal or gently inclined sediment layers deposited in front of the advancing forest beds of a delta.
A rounded rock more than 256 mm (10 inch) in diameter; larger than a cobblestone. See SOIL CLASSIFICATION.
Environmental conditions, e.g. waves, currents, drifts, etc. used as boundary input to physical or numerical models
A tide GAUGE that is operated by a float in a long vertical box to which the tide is admitted through an opening in the bottom. In the original type of box gauge the float supported a graduated rod which rose and fell with the tide.
A river type with multiple channels separated by shoals, bars and islands
(1) Formation of a channel through a barrier spit or island by storm waves, tidal action, or river flow. Usually occurs after a greater than normal flow, such as during a hurricane. (2) Failure of a dike allowing flooding.
A wave breaking on a shore, over a REEF, etc. Breakers may be classified into four types (See Figure II-4-1):
COLLAPSING--breaking occurs over lower half of wave, with minimal air pocket and usually no splash-up. Bubbles and foam present.
PLUNGING--crest curls over air pocket; breaking is usually with a crash. Smooth splash-up usually follows.
SPILLING--bubbles and turbulent water spill down front face of wave. The upper 25 percent of the front face may become vertical before breaking. Breaking generally occurs over quite a distance.
SURGING--wave peaks up, but bottom rushes forward from under wave, and wave slides up beach face with little or no bubble production. Water surface remains almost plane except where ripples may be produced on the beachface during runback.
The still-water depth at the point where a wave breaks. Also called BREAKING DEPTH.
Ratio of breaking wave height to DEEPWATER wave height
The zone within which waves approaching the coastline commence breaking, typically in water depths of between 5 and 10 meters for ocean coasts, but sometimes in shallower water.
Reduction in wave energy and height in the surf zone due to limited water depth
A man-made structure protecting a shore area, harbor, anchorage, or basin from waves. A harbor work.
Vertically-faced or steeply inclined structure usually built with timber and parallel to the shoreline, at or near the
beach crest, to resist erosion or mitigate against flooding.
A parcel or strip of land that is designed and designated to permanently remain vegetated in an undisturbed and
natural condition to protect an adjacent aquatic or wetland site from upland impacts, to provide habitat for wildlife and to
afford limited public access.
A structure or partition to retain or prevent sliding of the land. A secondary purpose is to protect the UPLAND
against damage from wave action.
Identical to apparent specific gravity, Ga = soil density ÷ density of water. “Apparent” means that the basis of
measurement is the total soil volume including voids, not just the individual soil particles.
Substantial lip or protuberance at the top of the seaward face of a wall, to deflect waves seaward.
A float; especially a floating object moored to the bottom, to mark a channel, anchor, shoal rock, etc. Some common types include: a nun or nut buoy is conical in shape; a can buoy is squat and cylindrical above water and conical below water; a spar buoy is a vertical, slender spar anchored at one end; a bell buoy, bearing a bell, runs mechanically or by the action of waves, usually marks shoals or rocks; a whistling buoy, similarly operated, marks shoals or channel entrances; a dan buoy carries a pole with a flag or light on it.
The resultant of upward forces, exerted by the water on a submerged or floating body, equal to the weight of the
water displaced by this body.
Hydraulic or mechanical movement of sand from the accreting updrift side to the eroding downdrift side of an inlet or harbor entrance. The hydraulic movement may include natural movement as well as movement caused by man.
Concrete box-type structure.
Containing calcium carbonate (CaCO3), chiefly as the minerals calcite and aragonite. When applied to rock, it implies that as much as 50 percent of the rock is carbonate (e.g., calcareous sand).
The condition of the water surface when there is no WIND WAVES or SWELL.
An artificial watercourse cut through a land area for such uses as navigation and irrigation.
A relatively narrow, deep depression with steep slopes, the bottom of which grades continuously downward. May be underwater (submarine) or on land (SUBAERIAL).
A land area jutting seaward from a continent or large island which prominently marks a change in, or interrupts notably, the coastal trend; a prominent feature. Examples: Cape Cod, Massachusetts; Cape Hatteras, North Carolina.
A wave whose velocity of propagation is controlled primarily by the surface tension of the liquid in which the wave is traveling. Water waves of length less than about 1 inch are considered capillary waves. Waves longer than 1 inch and shorter than 2 inches are in an indeterminate zone between capillary and gravity waves. See RIPPLE.
The science and art of making maps.
The area which drains naturally to a particular point on a river, thus contributing to its natural discharge.
A raised road across wet or marshy ground, or across water.
In refraction of waves, the name given to the curve to which adjacent orthogonals of waves refracted by a bottom whose contour lines are curved, are tangents. The occurrence of a caustic always marks a region of crossed orthogonals and high wave convergence.
CENTRAL PRESSURE INDEX (CPI)
The estimated minimum barometric pressure in the eye (approximate center) of a particular hurricane. The CPI is considered the most stable index to intensity of hurricane wind velocities in the periphery of the storm; the highest wind speeds are associated with storms having the lowest CPI.
(1) A natural or artificial waterway of perceptible extent which either periodically or continuously contains moving water, or which forms a connecting link between two bodies of water. (2) The part of a body of water deep enough to be used for navigation through an area otherwise too shallow for navigation. (3) A large strait, as the English Channel. (4) The deepest part of a stream, bay, or strait through which the main volume or current of water flows (see THALWEG).
The maximum flow which a channel is capable of transmitting without its banks being overtopped.
A bar built where a stream enters a body of standing water, resulting from decreased flow velocity.
CHARACTERISTIC WAVE HEIGHT
See SIGNIFICANT WAVE HEIGHT.
A special-purpose map, esp. one designed for navigation such as a bathymetric chart.
The plane or level to which soundings (or elevations) or tide heights are referenced (usually LOW WATER DATUM). The surface is called a tidal datum when referred to a certain phase of tide. To provide a safety factor for navigation, some level lower than MEAN SEA LEVEL is generally selected for hydrographic charts, such as MEAN LOW WATER or MEAN LOWER LOW WATER. See DATUM PLANE.
Disintegration of rocks and sediments by chemical alteration of the constituent minerals or of the cementing matrix. It is caused by exposure, oxidation, temperature changes, and biological processes.
A long, narrow wooded beach ridge or sandy hummock forming roughly parallel to a prograding shore, usually
seaward of marsh and mud-flat deposits (as along the south coast of Louisiana)
The short-crested waves that may spring up quickly in a moderate breeze, and which break easily at the crest. Also WIND CHOP.
Short, rough waves tumbling with a short and quick motion. Short-crested waves that may spring up quickly in a
moderate breeze, and break easily at the crest.
The French equivalent for a type of STANDING WAVE. In American usage it is usually associated with the standing wave phenomenon caused by the reflection of a nonbreaking wave train from a structure with a face that is vertical or nearly vertical. Full clapotis is one with 100 percent reflection of the incident wave; partial clapotis is one with less than 100 percent reflection.
Rocks built up of fragments which have been produced by weathering and erosion of pre-existing rocks and
minerals and, typically, transported mechanically to their point of deposition.
A fine grained, plastic, sediment with a typical grain size less than 0.004 mm. Possesses electromagnetic properties which bind the grains together to give a bulk strength or cohesion. See SOIL CLASSIFICATION.
A high, steep face of rock; a precipice. See also SEA CLIFF.
The characteristic weather of a region, particularly regarding temperature and precipitation, averaged over some significant internal of time (years).
The line dividing inland waters and the territorial sea at the mouth of a river, bay, or harbor.
The water depth beyond which repetitive profile or topographic surveys (collected over several years) do not detect vertical sea bed changes, generally considered the seaward limit of littoral transport. The depth can be determined from repeated cross-shore profile surveys or estimated using formulas based on wave statistics. Note that this does not imply the lack of sediment motion beyond this depth.
A type of wave in shallow water (i.e., where the depth of water is less than 1/8 to 1/10 the wavelength). The surface profile is expressed in terms of the Jacobian elliptic function cn u; hence the term cnoidal.
Lines which link all the points where TIDE is at the same stage (or phase) of its cycle.
(1) A strip of land of indefinite width (may be several kilometers) that extends from the SHORELINE inland to the first major change in terrain features. (See Figure A-1.) (2) The part of a country regarded as near the coast.
The land and sea area bordering the SHORELINE. (See Figure A-1)
(1) Those currents which flow roughly parallel to the shore and constitute a relatively uniform drift in the deeper water adjacent to the surf zone. These currents may be tidal currents, transient, wind-driven currents, or currents associated with the distribution of mass in local waters. (2) For navigational purposes, the term is used to designate a current in coastwise shipping lanes where the tidal current is frequently rotary.
General term used to encompass both coast protection against erosion and sea defense against flooding.
The natural processes which drive coastal hydro- and morphodynamics (e.g.winds, waves, tides, etc).
The plain composed of horizontal or gently sloping strata of clastic materials, generally representing a strip of sea bottom that has emerged from the sea in recent geologic time. May extend inland many km.
Collective term covering the action of natural forces on the SHORELINE, and near shore seabed
A zone directly adjacent to the waterline, where only coast related activities take place. Usually this is a strip of some 100 m wide. In this strip the coastal defense activities take place. In this strip often there are restrictions to land use.
The transition zone where the land meets water, the region that is directly influenced by marine and lacustrine hydrodynamic processes. Extends offshore to the continental shelf break and onshore to the first major change in topography above the reach of major storm waves. On barrier coasts, includes the bays and LAGOONS between the BARRIER and the mainland.
COASTAL ZONE MANAGEMENT
The integrated and general development of the coastal zone. Coastal Zone Management is not restricted to coastal defense works, but includes also a development in economical, ecological and social terms. Coastline Management is a part of Coastal Zone Management.
The term used in the Submerged Lands Act to describe the low-water line and closing lines across the mouths of
inland water bodies.
(1) Technically, the line that forms the boundary between the coast and the shore. (2) Commonly, the line that
forms the boundary between the land and the water, esp. the water of a sea or ocean. The SHORELINE. A more general
term than COAST LINE.
A rock fragment between 64 and 256 mm in diameter, usually rounded. See SOIL CLASSIFICATION.
A temporary watertight structure enclosing all or part of the construction area so that construction can proceed in
Sediment containing significant proportion of clays, the electromagnetic properties of which cause the sediment to bind together.
As a size term refers to particles smaller than 0.00024 mm, smaller than clay size.
(1) A DEEPWATER wave whose crest is pushed forward by a strong wind; much larger than a whitecap. (2) A
The ability of a wind or water current to transport detritus, in terms of particle size rather than amount, measured as the diameter of the largest particles.
A large RECURVED SPIT with secondary spits developed at its end. Example: Sandy Hook, New Jersey.
The junction of two or more river reaches or channels (the opposite of a bifurcation) .
The gradual, slow compression of a cohesive soil due to weight acting on it, which occurs as water is driven out of the voids in the soil. Consolidation only occurs in clays or other soils of low permeability.
(1) The zone bordering a continent extending from the line of permanent immersion to the depth, usually about 100 m to 200 m, where there is a marked or rather steep descent toward the great depths of the ocean. (2) The area under active littoral processes during the HOLOCENE period. (3) The region of the oceanic bottom that extends outward from the shoreline with an average slope of less than 1:100, to a line where the gradient begins to exceed 1:40 (the CONTINENTAL SLOPE).
The declivity from the offshore border of the CONTINENTAL SHELF to oceanic depths. It is characterized by a marked increase in slope.
A line on a map or chart representing points of equal elevation with relation to a DATUM. It is called an ISOBATH when connecting points of equal depth below a datum. Also called DEPTH CONTOUR.
The least depth in the navigable parts of a waterway, governing the maximum draft of vessels that can enter.
(1) In refraction phenomena, the decreasing of the distance between orthogonals in the direction of wave travel. Denotes an area of increasing wave height and energy concentration. (2) In wind-setup phenomena, the increase in setup observed over that which would occur in an equivalent rectangular basin of uniform depth, caused by changes in planform or depth; also the decrease in basin width or depth causing such increase in setup.
(1) (Biology) Marine coelenterates (Madreporaria), solitary or colonial, which form a hard external covering of calcium compounds or other materials. The corals which form large REEFS are limited to warm, shallow waters, while those forming solitary, minute growths may be found in colder waters to great depths. (2) (Geology) The concretion of coral polyps, composed almost wholly of calcium carbonate, forming reefs and tree-like and globular masses. May also include calcareous algae and other organisms producing calcareous secretions, such as bryozoans and hydrozoans.
A coral-algal mound or ridge of in-place coral colonies and skeletal fragments, carbonate sand, and organically-secreted calcium carbonate. A coral reef is built up around a wave-resistant framework, usually of older coral colonies.
(1) A cylindrical sample extracted from a beach or seabed to investigate the types and depths of sediment layers.
(2) An inner, often much less permeable portion of a BREAKWATER or BARRIER BEACH
Force due to the Earth's rotation, capable of generating currents. It causes moving bodies to be deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. The "force" is proportional to the speed and latitude of the moving object. It is zero at the equator and maximum at the poles.
A small, sheltered recess in a COAST, often inside a larger EMBAYMENT.
The outer layer used in a rubble system as protection against external hydraulic loads
(1) A stream, less predominant than a river, and generallytributary to a river. (2) A small tidal channel through a coastal MARSH.
Very slow, continuous downslope movement of soil or debris.
An indented or wavy shoreline beach form, with the regular seaward- pointing parts rounded rather than sharp, as in the cuspate type.
Highest point on a beach face, BREAKWATER, or SEAWALL.
CREST LENGTH, WAVE
The length of a wave along its crest. Sometimes called CREST WIDTH.
CREST OF WAVE
(1) the highest part of a wave. (2) That part of the wave above still-water level. (See Figure II-1-4.)
CREST OF BERM
The seaward limit of a berm. Also called BERM EDGE. (See Figure A-1.)
CREST WIDTH, WAVE
See CREST LENGTH, WAVE.
An arrangement of relatively thin layers of rock inclined at an angle to the more nearly horizontal BEDDING
PLANES of the larger rock unit. Also referred to as cross-stratification.
Perpendicular to the SHORELINE.
Concrete superstructure on a rubble mound.
(1) The flowing of water, or other liquid or gas. (2) That portion of a stream of water which is moving with a velocity much greater than the average or in which the progress of the water is principally concentrated. (3) Ocean currents can be classified in a number of different ways. Some important types include the following: (1) Periodic - due to the effect of the tides; such Currents may be rotating rather than having a simple back and forth motion. The currents accompanying tides are known as tidal currents; (2) Temporary - due to seasonal winds; (3) Permanent or ocean - constitute a part of the general ocean circulation. The term DRIFT CURRENT is often applied to a slow broad movement of the oceanic water; (4) Nearshore - caused principally by waves breaking along a shore.
One of the offshore currents flowing generally parallel to the shoreline in the deeper water beyond and near the surf zone; these are not related genetically to waves and resulting surf, but may be related to tides, winds, or distribution of mass.
A broad, shallow, slow-moving ocean or lake current. Opposite of CURRENT, STREAM.
The tidal current away from shore or down a tidal stream. Usually associated with the decrease in the height of the tide.
Any of the parts of the nearshore current system that flow parallel to shore before converging and forming the neck of the RIP CURRENT.
The tidal current toward shore or up a tidal stream. Usually associated with the increase in the height of the tide.
See INSHORE CURRENT.
Any current in the littoral zone caused primarily by wave action; e.g., LONGSHORE CURRENT, RIP CURRENT. See also CURRENT, NEARSHORE.
The littoral current in the breaker zone moving essentially parallel to the shore, usually generated by waves breaking at an angle to the shoreline.
An instrument for measuring the velocity of a current
A current in the NEARSHORE ZONE. (See Figure A-1)
See OFFSHORE CURRENT.
See CURRENT, TIDAL.
See PERMANENT CURRENT.
See RIP CURRENT.
A narrow, deep, and swift ocean current, as the Gulf Stream. CURRENT, DRIFT.
CURRENT SYSTEM, NEARSHORE
See NEARSHORE CURRENT SYSTEM.
The alternating horizontal movement of water associated with the rise and fall of the tide caused by the astronomical tide-producing forces. Also CURRENT, PERIODIC. See also CURRENT, FLOOD and CURRENT, EBB.
Process by which wave velocity, height, and direction are affected by a current
One of a series of short ridges on the FORESHORE separated by crescent-shaped troughs spaced at more or less regular intervals. Between these cusps are hollows. The cusps are spaced at somewhat uniform distances along beaches. They represent a combination of constructive and destructive processes. Also BEACH CUSP. (See Figure III-2-23.)
A crescent-shaped bar uniting with the shore at each end. It may be formed by a single spit growing from shore and then turning back to again meet the shore, or by two spits growing from the shore and uniting to form a bar of sharply cuspate form.
The spit that forms in the lee of a shoal or offshore feature (BREAKWATER, island, rock outcrop) by waves that are refracted and/or diffracted around the offshore feature. It may eventually grow into a TOMBOLO linking the feature to the mainland.
A hydraulic dredge that uses a rotating steel head consisting of hardened cutting blades and a backing ring to
dislodge bottom material. The head is mounted at the suction entrance of the hydraulic pipeline, and fluidized material is
picked up by suction and carried away through the pipe.
A steep, symmetrical wave whose crest forms an angle of 120 degrees and whose form is that of a cycloid. A
trochoidal wave of maximum steepness. See also TROCHOIDAL WAVE.
A system of winds that rotates about a center of low atmospheric pressure. Rotation is clockwise in the Southern
Hemisphere and anti-clockwise in the Northern Hemisphere. In the Indian Ocean, the term refers to the powerful storms
called HURRICANES in the Atlantic.
Structure built in rivers or estuaries, basically to separate water at both sides and/or to retain water at one side.
Any permanent line, plane or surface used as a reference datum to which elevations are referred.
See CHART DATUM.
The horizontal plane to which soundings, ground elevations, or water surface elevations are referred. Also REFERENCE PLANE. The plane is called a TIDAL DATUM when defined by a certain phase of the tide. The following datums are ordinarily used on hydrographic charts:
MEAN LOW WATER--Atlantic coast (U. S.), Argentina, Sweden, and Norway.
MEAN LOWER LOW WATER--Pacific coast (U. S.).
MEAN LOW WATER SPRINGS--United Kingdom, Germany, Italy, Brazil, and Chile.
LOW WATER DATUM--Great Lakes (U. S. and Canada).
LOWEST LOW WATER SPRINGS--Portugal.
LOW WATER INDIAN SPRINGS--India and Japan (See INDIAN TIDE PLANE).
LOWEST LOW WATER--France, Spain, and Greece.
A common datum used on United States topographic maps is MEAN SEA LEVEL. See also BENCH MARK.
Deep-ocean boundary current off the west coast of the U.S. which brings warmer, saltier, low oxygen, high phosphate equatorial type water from low to high latitudes.
A line near the limit of storm wave uprush marking the landward limit of debris deposits.
Area of relative CALM through which waves travel after emerging from the generating area.
The distance waves travel after leaving the generating area (FETCH).
DECAY OF WAVES
The change waves undergo after they leave a generating area (FETCH) and pass through a calm, or region of lighter winds. In the process of decay, the significant wave height decreases and the significant wavelength increases.
Water so deep that surface waves are little affected by the ocean bottom. Generally, water deeper than one-half the surface wavelength is considered deep water. Compare SHALLOW WATER.
DEEP WATER WAVES
A wave in water the depth of which is greater than one-half the WAVE LENGTH.
The removal of loose material from a beach or other land surface by wind action.
The geologic process by means of which various parts of the surface of the earth are worn away and their general level lowered, by the action of wind and water.
(1) An ALLUVIAL DEPOSIT, usually triangular or semi-circular, at the mouth of a river or stream. The delta is normally built up only where there is no tidal or current action capable of removing the sediment at the same rate as it is deposited, and hence the delta builds forward from the coastline. (2) A TIDAL DELTA is a similar deposit at the mouth of a tidal INLET, the result of TIDAL CURRENTS that flow in and out of the inlet.
The nearly-level surface composing the landward portion of a large DELTA.
Mass (in kg) per unit of volume of a substance; kg/m3. For pure water, the density is 1000 kg/m3, for seawater the density is usually more. Density increases with increasing salinity, and decreases with increasing temperature. More information can be found in "properties of seawater". For stone and sand, usually a density of 2600 kg/m3 is assumed. Concrete is less dense, in the order of 2400 kg/m3. Some types of basalt may reach 2800 kg/m3. For sand, including the voids, one may use 1600 kg/m3, while mud often has a density of 1100 - 1200 kg/m3.
Phenomenon of relative flow within water due to difference in density. For example, the salt-water wedge is a
density current, as is a volcanic nuée ardente.
The lateral expansion of a sediment plume as it moves out of the distributary mouth, where salt and fresh water mix. This is most likely to occur where the speed of the river flow is moderate to low and the distributary mouth is relatively deep.
Variations in salinity create variations in density in estuaries. These variations in density create horizontal pressure gradients, which drive estuarine circulation.
A general term signifying any depressed or lower area in the ocean floor.
The vertical distance from a specified datum to the sea floor.
See CONTOUR, also ISOBATH.
See CONTROLLING DEPTH.
See SHOALING COEFFICIENT.
DEPTH OF BREAKING
The still-water depth at the point where the wave breaks. Also BREAKER DEPTH.
See STONE, DERRICK.
See HYPOTHETICAL HURRICANE.
A hypothetical extreme storm whose waves coastal protection structures will often be designed to withstand. The severity of the storm (i.e. return period) is chosen in view of the acceptable level of risk of damage or failure. A DESIGN STORM consists of a DESIGN WAVE condition, a design water level and a duration.
In the design of HARBORS, harbor works, etc., the type or types of waves selected as having the characteristics against which protection is desired.
DESIGN WAVE CONDITION
Usually an extreme wave condition with a specified return period used in the design of coastal works.
A BREAKWATER without any SUBAERIAL connection to the shore.
Small fragments of rock which have been worn or broken away from a mass by the action of water or waves.
DIFFERENTIAL EROSION / WEATHERING
These features develop in rocks which have varying resistance to the agencies of erosion and/or weathering so that parts of the rock are removed at greater rates than others. A typical example is the removal of soft beds from between harder beds in a series of sedimentary rocks. The term may be applied to any size of feature, from small-scale ‘etching’ to the regional development of hills and valleys controlled by hard and soft rocks.
DIFFRACTION (of water waves)
The phenomenon by which energy is transmitted laterally along a wave crest. When a part of a train of waves is interrupted by a barrier, such as a BREAKWATER, the effect of diffraction is manifested by propagation of waves into the sheltered region within the barrier's geometric shadow. (See Figure II-7-2)
Ratio of diffracted wave height to DEEPWATER wave height.
The distributing or spreading-out of molecules, atoms, or substances into a vacuum, fluid, or porous medium so that the concentration equalizes in all parts of the system
Earth structure along sea or river in order to protect low lands from flooding by high water; dikes along rivers are sometimes called LEVEES. Sometimes written as DYKE
The volume of water per unit of time flowing along a pipe or channel.
(1) Pattern of geographic distribution of individuals within a species. (2) Distortion of the shape of a seismic wave train or ocean wave train because of variations of velocity with frequency.
Multiple branches of a river.
A channel to convey water for irrigation or drainage.
Having a period or cycle of approximately one TIDAL DAY.
The type of tidal current having only one FLOOD and one EBB period in the tidal day. A ROTARY CURRENT is diurnal if it changes its direction through all points of the compass once each tidal day.
The difference in height of the two high waters or of the two low waters of each day. Also, the difference in velocity between the two daily flood or EBB CURRENTS of each day.
A tide with one high water and one low water in a tidal day. (See Figure II-5-16)
(1) In refraction phenomena, the increasing of distance between orthogonals in the direction of wave travel. Denotes an area of decreasing wave height and energy concentration. (2) In wind-setup phenomena, the decrease in setup observed under that which would occur in an equivalent rectangular basin of uniform depth, caused by changes in planform or depth. Also the increase in basin width or depth causing such decrease in setup.
Waves that move obliquely out from a vessel’s sailing line. (See Figure II-7-40)
A waterway used to divert water from its natural course. The term is generally applied to a temporary arrangement
e.g. to by-pass water around a dam site during construction.
The slip or waterway between two piers, or cut into the land, for the reception of ships.
A cluster of piles.
The direction of predominant movement of littoral materials.
Along coasts with obliquely approaching waves there is a longshore (wave-driven) current. For this current, one can define an upstream and a DOWNSTREAM direction. For example, on a beach with an orientation west-east, the sea is to the north. Suppose the waves come from NW, then the current flows from West to East. Here, UPSTREAM is west of the observer, and east is downstream of the observer.
A downward movement (sinking) of surface water caused by onshore Ekman transport, converging CURRENTS, or when a water mass becomes more dense than the surrounding water.
Total area drained by a stream and its tributaries.
An artificially maintained sea lane extending from an inland water body into the marginal sea to accomodate vessel traffic through coastal shallows.
DREDGED MATERIAL PLACEMENT SITE
Designated area for dredged material placement. In the United States, designated areas must be coordinated with the Environmental Protection Agency and resource agencies such as the U. S. Fish and Wildlife Service and the National marine Fisheries Service for environmental compliance and with local interests for capacity and acceptability.
The practice of excavating or displacing the bottom or shoreline of a water body. Dredging can be accomplished with mechanical or hydraulic machines. Most is done to maintain channel depths or berths for navigational purposes; other dredging is for shellfish harvesting, for cleanup of polluted sediments, and for placement of sand on beaches.
(1) Sometimes used as a short form for LITTORAL DRIFT. (2) The speed at which a current runs. (3) Floating material deposited on a beach (driftwood). (4) A deposit of a continental ice sheet; e.g., a DRUMLIN.
A broad, shallow, slow-moving ocean or lake current.
A particular reach of marine shore in which LITTORAL DRIFT may occur without significant interruption, and which contain any and all natural sources of such drift, and also any accretion shore forms accreted by such drift.
A large medieval fast-sailing galley or cutter.
A shore with long, narrow channels, implying that subsidence of the coast has transformed the lower portions of river valleys into tidal estuaries.
A low, smoothly-rounded, elongate hill of compact glacial till built under the margin of the ice and shaped by its flow.
That part of the beach which is uncovered by water (e.g. at low tide). Sometimes referred to as 'SUBAERIAL' beach.
(1) Ridges or mounds of loose, wind-blown material, usually sand. (See Figure IV-2-11.) (2) Bed forms smaller than bars but larger than ripples that are out of phase with any water-surface gravity waves associated with them.
The ability of a rock to retain its physical and mechanical properties (i.e. resist degradation) in engineering service.
In wave forecasting, the length of time the wind blows in nearly the same direction over the FETCH (generating
The time necessary for steady-state wave conditions to develop for a given wind velocity over a given fetch length.
DURATION OF EBB
The interval of time in which a tidal current is ebbing, determined from the middle of the slack waters.
DURATION OF FALL
The interval from high water to low water.
DURATION OF FLOOD
The interval of time in which a tidal current is flooding, determined from the middle of slack waters.
DURATION OF RISE
The interval from low water to high water.
Short term morphological changes that do not affect the morphology over a long period.
In fluid dynamics, the ratio between the shear stress acting along any plane between neighboring fluid elements and the rate of deformation of the velocity gradient perpendicular to this plane.
Period when tide level is falling; often taken to mean the ebb current which occurs during this period.
The movement of a tidal current away from shore or down a tidal stream. In the semidiurnal type of reversing current, the terms greater ebb and lesser ebb are applied respectively to the ebb currents of greater and lesser velocity of each day. The terms of maximum ebb and minimum ebb are applied to the maximum and minimum velocities of a continuously running ebb current, the velocity alternately increasing and decreasing without coming to a slack or reversing. The expression maximum ebb is also applicable to any ebb current at the time of greatest velocity.
The interval between the transit of the moon over the meridian of a place and the time of the following strength of ebb.
High, landward margin of a flood-tidal shoal that helps divert ebb-tide currents around the shoal.
The EBB CURRENT at the time of maximum velocity.
EBB TIDAL DELTA
The bulge of sand formed at the seaward mouth of TIDAL INLETS as a result of interaction between tidal currents and waves. Also called inlet-associated bars and estuary entrance shoals.
The period of tide between high water and the succeeding low water; a falling tide. (See Figure II-5-16.)
An electronic instrument used to determine the depth of water by measuring the time interval between the emission of a sonic or ultrasonic signal and the return of its echo from the bottom.
The living organisms and the nonliving environment interacting in a given area, encompassing the relationships between biological, geochemical, and geophysical systems.
A circular movement of water formed on the side of a main current. Eddies may be created at points where the main stream passes projecting obstructions or where two adjacent currents flow counter to each other.
An ocean wave parallel to a coast, with crests normal to the shoreline. An edge wave may be STANDING or PROGRESSIVE. Its height diminishes rapidly seaward and is negligible at a distance of one wavelength offshore.
Resultant flow at right angles to and to the right of the wind direction (in the northern hemisphere) referred to as UPWELLING and DOWNWELLING.
The vertical distance from mean sea level or other established datum plane to a point on the earth’s surface; height above sea level. Although sea floor elevation below msl should be marked as a negative value, many charts show positive numerals for water depth.
Warm equatorial water which flows southward along the coast of Peru and Ecuador during February and March of certain years. It is caused by poleward motions of air and unusual water temperature patterns in the Pacific Ocean, which cause coastal downwelling, leading to the reversal in the normal north-flowing cold coastal currents. During many El Niño years, storms, rainfall, and other meteorological phenomena in the Western Hemisphere are measurably different than during non-El Niño years.
The process by which a granular material can be sorted into its constituent particle sizes by means of a moving
stream of fluid (usually air or water). Elutriators are extensively used in studies of sediments for determining Particle size
distribution. Under certain circumstances wind, rivers and streams may act as elutriating agents.
Fill material, usually earth or rock, placed with sloping sides and with a length greater than its height. Usually an embankment is wider than a dike.
An indentation in the shore forming an open bay.
A coast in which land formerly under water has recently been exposed above sea level, either by uplift of the land or by a drop in sea level.
Native or confined to a specific geographic area.
The ratio of the energy in a wave per unit crest length transmitted forward with the wave at a point in shallow water to the energy in a wave per unit crest length transmitted forward with the wave in deep water. On refraction diagrams this is equal to the ratio of the distance between a pair of orthogonals at a selected shallow-water point to the distance between the same pair of orthogonals in deep water. Also the square of the REFRACTION COEFFICIENT.
The avenue of access or opening to a navigable channel or inlet.
EOLIAN (also AEOLIAN)
Pertaining to the wind, esp. used with deposits such as loess and dune sand, and sedimentary structures like wind-formed ripple marks.
Sediments of sand size or smaller which have been transported by winds. They may be recognized in marine
deposits off desert coasts by the greater angularity of the grains compared with waterborne particles.
- Ocean currents flowing westerly near the equator. There are two such currents in both the Atlantic and Pacific Oceans. The one to the north of the equator is called the North Equatorial Current and the one to the south is called the South Equatorial Current. Between these two currents there is an easterly flowing stream known as the Equatorial Countercurrent.
- Tidal currents occurring semimonthly as a result of the moon being over the equator. At these times the tendency of the moon to produce DIURNAL INEQUALITY in the current is at a minimum.
Tides occurring semimonthly as the result of the moon being over the equator. At these times the tendency of the moon to produce a DIURNAL INEQUALITY in the tide is at a minimum.
The wearing away of land by the action of natural forces. On a beach, the carrying away of beach material by wave action, tidal currents, littoral currents, or by deflation.
A more or less continuous line of cliffs or steep slopes facing in one general direction which are caused by erosion or faulting. Also SCARP. (See Figure A-1)
(1) The part of a river that is affected by tides. (2) The region near a river mouth in which the fresh water of the river mixes with the salt water of the sea and which received both fluvial and littoral sediment influx.
EUSTATIC SEA LEVEL CHANGE
Change in the relative volume of the world’s ocean basins and the total amount of ocean water.
In meteorology, usually the "eye of the storm" (hurricane): the roughly circular area of comparatively light winds and fair weather found at the center of a severe tropical cyclone.
The parts of a waterway that are open and unobstructed for navigation. The main traveled part of a waterway; a
The frequency band (nominally 0.001 - 0.02 Hz) occupied by SHEAR INSTABILITIES of the longshore current. This band falls both below and in the lower part of the Infragravity band occupied by Infragravity waves.
A unit of measurement used for soundings equal to 1.83 meters (6 feet).
The copyrighted trademark for a type of ECHO SOUNDER.
A fracture in rock along which there has been an observable amount of displacement. Faults are rarely single planar units; normally they occur as parallel to sub-parallel sets of planes along which movement has taken place to a greater or lesser extent. Such sets are called fault or fracture-zones.
The entire group of animals found in an area.
An artificially widened beach serving to nourish downdrift beaches by natural littoral currents or forces.
The currents which flow parallel to shore before converging and forming the neck of a RIP CURRENT.
See CURRENT, FEEDER.
The initial action of a deepwater wave, in response to the bottom, upon running into shoal water.
The area in which SEAS are generated by a wind having a fairly constant direction and speed. Sometimes used
synonymously with FETCH LENGTH. Also GENERATING AREA.
The horizontal distance (in the direction of the wind) over which a wind generates seas or creates a WIND SETUP.
Situation in which wave energy (or wave height) is limited by the size of the wave generation area (fetch).
Intermediate layer, preventing fine materials of an underlayer from being washed through the voids of an upper
A narrow, deep, steep-walled inlet of the sea, usually formed by entrance of the sea into a deep glacial trough.
A narrow arm of the sea; also, the opening of a river into the sea.
(1) Period when tide level is rising; often taken to mean the flood current which occurs during this period (2) A flow beyond the carrying capacity of a channel.
Channel located on ebb-tidal shoal that carries the flood tide over the tidal flat into the back bay or lagoon.
The movement of a tidal current toward the shore or up a tidal stream. In the semidiurnal type of reversing current, the terms greater flood and lesser flood are applied respectively to the flood currents of greater and lesser velocity each day. The terms maximum flood and minimum flood are applied to the maximum and minimum velocities of a flood current the velocity of which alternately increases and decreases without coming to slack or reversing. The expression maximum flood is also applicable to any flood current at the time of greatest velocity.
A gravity outlet fitted with vertically-hinged doors, opening if the inner water level is higher than the outer water level, so that drainage takes place during low water.
The interval between the transit of the moon over the meridian of a place and the time of the following flood.
Proof of any kind on the shoreline, or on structures like bridge abutments, used to determine the highest level attained by the water surface during the flood (note: the height of the flood mark usually includes the wave run-up).
1) A flat tract of land bordering a river, mainly in its lower reaches, and consisting of ALLUVIUM deposited by the river. It is formed by the sweeping of the meander belts downstream, thus widening the valley, the sides of which may become some kilometers apart. In time of flood, when the river overflows its banks, sediment is deposited along the valley banks and plains. (2) Synonymous with 100-year floodplain. The land area susceptible to being inundated by stream derived waters with a 1 percent chance of being equaled or exceeded in any given year.
Seaward-dipping sand platform dominated by flood-tidal currents, located on ebb-tidal shoal near the opening to the inlet.
The determination of the attenuating effect of storage on a river-flood passing through a valley by reason of a feature acting as control (e.g. a reservoir with a spillway capacity less than the flood inflow, or the widening or narrowing of a valley).
FLOOD TIDAL DELTA
The bulge of sand formed at the landward mouth of TIDAL INLETS as a result of flow expansion.
The period of tide between low water and the succeeding high water; a rising tide. (See Figure II-5-16.)
FLOOD WALL, SPLASH WALL
Wall, retired from the seaward edge of the seawall crest, to prevent water from flowing onto the land behind.
The entire group of plants found in an area.
Of or pertaining to rivers; produced by the action of a river or stream (e.g., fluvial sediment).
The time required to replace all the water in an ESTUARY, HARBOR, etc., by action of current and tide.
(1) The front of a wave as it advances shoreward, after it has broken. (2) Lines of foam such as those which move around the head of a RIP.
Generally, the same as a tailwind; in wave forecasting, wind blowing in the direction of ocean-wave advance.
The front DUNE immediately behind the backshore.
Low, long-period ocean SWELL which commonly precedes the main swell from a distant storm, especially a
The part of the shore, lying between the crest of the seaward berm (or upper limit of wave wash at high tide) and the ordinary low-water mark, that is ordinarily traversed by the uprush and backrush of the waves as the tides rise and fall. See BEACH FACE. (See Figure A-1)
The seaward side of a REEF (usually coral); in places a steep slope covered with reef talus.
FORWARD SPEED (hurricane)
Rate of movement (propagation) of the hurricane eye in meters per second, knots, or miles per hour.
At a given time, the vertical distance between the water level and the top of the structure. On a ship, the distance
from the waterline to main deck or gunwale.
A series of islands that fringe, or mask, a mainland coast often known as BARRIER ISLANDS. The waters
landward of such islands are sometimes treated as high seas enclaves or as inland waters.
A coral REEF attached directly to an insular or continental shore. There may be a shallow channel or lagoon
between the reef and the adjacent mainland.
FRONT OF THE FETCH
In wave forecasting, the end of the generating area toward which the wind is blowing.
The dimensionless ratio of the inertial force to the force of gravity for a given fluid flow. It may be given as Fr = V /Lg where V is a characteristic velocity, L is a characteristic length, and g the acceleration of gravity - or as the square root of this number.
The waves that form when wind blows for a sufficient period of time across the open ocean. The waves of a fully developed sea have the maximum height possible for a given wind speed, FETCH and duration of wind.
(1) Steel wire-mesh basket to hold stones or crushed rock to protect a bank or bottom from erosion. (2) Structures composed of masses of rocks, rubble or masonry held tightly together usually by wire mesh so as to form blocks or walls. Sometimes used on heavy erosion areas to retard wave action or as a foundation for BREAKWATERS or JETTIES.
A wind between a strong breeze and a storm. A continuous wind blowing in degrees of moderate, fresh, strong, or whole gale and varying in velocity from 28 to 47 nautical miles per hour (see BEAUFORT SCALE).
Instrument for measuring the water level relative to a datum or for measuring other parameters.
In wave forecasting, the continuous area of water surface over which the wind blows in nearly a constant direction. Sometimes used synonymously with FETCH LENGTH. Also FETCH.
GEOGRAPHICAL INFORMATION SYSTEM (GIS)
Database of information which is geographically referenced, usually with an associated visualization system.
Unit of linear measure equal to one minute of latitude at the equator. See NAUTICAL MILE.
GEOMETRIC MEAN DIAMETER
The diameter equivalent of the arithmetic mean of the logarithmic frequency distribution. In the analysis of beach sands, it is taken as that grain diameter determined graphically by the intersection of a straight line through selected boundary sizes, (generally points on the distribution curve where 16 and 84 percent of the sample is coarser by weight) and a vertical line through the median diameter of the sample.
In wave diffraction theory, the area outlined by drawing straight lines paralleling the direction of wave approach through the extremities of a protective structure. It differs from the actual protected area to the extent that the diffraction and refraction effects modify the wave pattern.
(1) That branch of physical geography which deals with the form of the Earth, the general configuration of its surface, the distribution of the land, water, etc. (2) The investigation of the history of geologic changes through the interpretation of topographic forms.
The study of the physical characteristics and properties of the earth, usually employing quantitative physical methods.
A synthetic fabric which may be woven or non-woven used as a filter.
A large body of ice moving slowly down a slope of valley or spreading outward on a land surface (e.g., Greenland, Antarctica) and surviving from year to year.
The state of hydrostatic equilibrium of the earth’s crust as influenced by the weight of glacier ice.
GLOBAL POSITIONING SYSTEM (GPS)
A navigational and positioning system developed by the U.S. Department of Defense, by which the location of a
position on or above the Earth can be determined by a special receiver at that point interpreting signals received
simultaneously from several of a constellation of special satellites.
(1) The deepest portion of an inlet, the THROAT. (2) A narrow, deep valley with nearly vertical rock walls.
An arrangement of particle sizes within a single bed, with coarse grains at the bottom of the bed and progressively finer grains toward the top of the bed.
(1) A measure of slope (soil- or water-surface) in meters of rise or fall per meter of horizontal distance. (2) More general, a change of a value per unit of distance, e.g. the gradient in longshore transport causes erosion or accretion. (3) With reference to winds or currents, the rate of increase or decrease in speed, usually in the vertical; or the curve that represents this rate.
Distribution, with regard to size or weight, of individual stones within a bulk volume; heavy, light and fine grading are distinguished.
GRADUAL CLOSURE METHOD
Method in which the final closure gap in a dam is closed gradually either by the vertical or horizontal closure
method; this in contradiction with a sudden closure.
Band of granular material which is incorporated in an embankment, dam, dike, or bottom protection and is graded so as to allow seepage to flow across or down the filter zone without causing the migration of the material adjacent to the filter.
Unconsolidated natural accumulation of rounded rock fragments coarser than sand but finer than pebbles (2-4 mm diameter).
A wave whose velocity of propagation is controlled primarily by gravity. Water waves more than 5 cm long are
considered gravity waves. Waves longer than 2.5 cm and shorter than 5 cm are in an indeterminate zone between
CAPILLARY and GRAVITY WAVES. See RIPPLE.
GROIN (British, GROYNE)
Narrow, roughly shore-normal structure built to reduce longshore currents, and/or to trap and retain littoral material. Most groins are of timber or rock and extend from a SEAWALL, or the backshore, well onto the foreshore and rarely even further offshore. See T-GROIN, PERMEABLE GROIN, IMPERMEABLE GROIN.
The beach compartment between two groins.
A series of groins acting together to protect a section of beach. Commonly called a GROIN field.
A relatively large portion of the ocean or sea extending far into land; the largest of various forms of inlets of the sea (e.g., Gulf of Mexico, Gulf of Aqaba).
A tidal stream connecting two larger waterways.
A zone in which salinity changes rapidly.
A plane midway between MEAN HIGH WATER and MEAN LOW WATER, also called MEAN TIDE LEVEL.
HARBOR (British, HARBOUR)
Any protected water area affording a place of safety for vessels. See also PORT. A harbor may be natural or
HARBOR OSCILLATION (HARBOR SURGING)
The nontidal vertical water movement in a harbor or bay. Usually the vertical motions are low; but when oscillations are excited by a tsunami or storm surge, they may be quite large. Variable winds, air oscillations, or surf beat also may cause oscillations. See SEICHE.
General term applied to impermeable coastal defense structures of concrete, timber, steel, masonry, etc, which
reflect a high proportion of incident wave energy.
HEAD OF RIP
The part of a rip current that has widened out seaward of the breakers. See also CURRENT, RIP; CURRENT,
FEEDER; and NECK (RIP).
(1) A comparatively high promontory with either a CLIFF or steep face extending out into a body of water, such as a sea or lake. An unnamed HEAD is usually called a headland. (2) The section of RIP CURRENT which has widened out seaward of the BREAKERS, also called HEAD OF RIP. (3) Seaward end of BREAKWATER or dam.
The level of water in the reservoir.
(1) The vertical rise or fall of the waves or the sea. (2) The translational movement of a craft parallel to its vertical axis. (3) The net transport of a floating body resulting from wave action.
This term, in municipal and international law, denotes the continuous body of salt water in the world that is
navigable in its character and that lies outside territorial waters and maritime belts of the various countries.
HIGH TIDE, HIGH WATER (HW)
The maximum elevation reached by each rising tide. See TIDE. (See Figure II-5-16.)
HIGH WATER (HW)
Maximum height reached by a rising tide. The height may be solely due to the periodic tidal forces or it may have superimposed upon it the effects of prevailing meteorological conditions. Nontechnically, also called the HIGH TIDE.
HIGH WATER LINE
In strictness, the intersection of the plane of mean high water with the shore. The shoreline delineated on the nautical charts of the National Ocean Service is an approximation of the high water line. For specific occurrences, the highest elevation on the shore reached during a storm or rising tide, including meteorological effects.
HIGH WATER MARK
A reference mark on a structure or natural object, indicating the maximum stage of tide or flood.
HIGH WATER OF ORDINARY SPRING TIDES (HWOST)
A tidal datum appearing in some British publications, based on high water of ordinary spring tides.
HIGHER HIGH WATER (HHW)
The higher of the two high waters of any tidal day. The single high water occurring daily during periods when the tide is diurnal is considered to be a higher high water. (See Figure II-5-16.)
HIGHER LOW WATER (HLW)
The higher of two low waters of any tidal day. (See Figure II-5-16.)
HIGHEST ASTRONOMICAL TIDE (HAT)
The highest level of water which can be predicted to occur under any combination of astronomical conditions. This level may not be reached every year.
In wave prediction, the retrospective forecasting of waves using measured wind information.
The region lying inland from the coast. Also the inland area served by a port.
HISTORIC EVENT ANALYSIS
Extreme analysis based on hindcasting typically ten events over a period of 100 years.
An epoch of the QUATERNARY period, from the end of the PLEISTOCENE, about 8,000 years ago, to the present time. Syn: Recent.
A condition in which the outflow jet from a river or coastal inlet and the water in the receiving basin are of the same density or are vertically mixed.
A spit or narrow cape of sand or gravel which turns landward at the outer end; a RECURVED SPIT.
Self-propelled floating plant which is capable of dredging material, storing it onboard, and transporting and placing the material at a specified disposal site. Often used to dredge inlets and then deposit the material along the open coast or offshore.
HORIZONTAL CLOSURE METHOD
Construction of a dam by dumping the materials from one or both banks, thus constricting the channel progressively laterally until the dam is closed. This method is also known as end dumping and point tipping
An intense tropical cyclone in which winds tend to spiral inward toward a core of low pressure, with maximum surface wind velocities that equal or exceed 33.5 m/sec (75 mph or 65 knots) for several minutes or longer at some points. TROPICAL STORM is the term applied if maximum winds are less than 33.5 m/sec but greater than a whole gale (63 mph or 55 knots). Term is used in the Atlantic, Gulf of Mexico, and eastern Pacific.
HURRICANE PATH or TRACK
Line of movement (propagation) of the eye through an area.
HURRICANE STAGE HYDROGRAPH
A continuous graph representing water level stages that would be recorded in a gage well located at a specified point of interest during the passage of a particular hurricane, assuming that effects of relatively short-period waves are eliminated from the record by damping features of the gage well. Unless specifically excluded and separately accounted for, hurricane surge hydrographs are assumed to include effects of astronomical tides, barometric pressure differences, and all other factors that influence water level stages within a properly designed gage well located at a specified point.
HURRICANE WIND PATTERN or ISOVEL PATTERN
An actual or graphical representation of near-surface wind velocities covering the entire area of a hurricane at a particular instant. Isovels are lines connecting points of simultaneous equal wind velocities, usually referenced 9 meters (30 feet) above the surface, in meters per second, knots, or meters per hour; wind directions at various points are indicated by arrows or deflection angles on the isovel charts. Isovel charts are usually prepared at each hour during a hurricane, but for each half hour during critical periods.
Floating or (occasionally) truck-based plant which lifts the material through a suction pipe. It requires dilution water for material pickup, lift, and transportation. Often used to renourish beaches when material is pumped onto the shore from an offshore sand source.
Quotient of the wetted cross-sectional area and the wetted perimeter.
HYDRAULICALLY EQUIVALENT GRAINS
Sedimentary particles that settle at the same rate under the same conditions.
(1) The description and study of seas, lakes, rivers and other waters. (2) The science of locating aids and dangers to navigation. (3) The description of physical properties of the waters of a region.
The pressure exerted by water at any given point in a body of water at rest.
Outflow from a river or coastal inlet in which a wedge of less dense water flows over the denser sea water.
HYPOTHETICAL HURRICANE ("HYPOHURRICANE")
A representation of a hurricane, with specified characteristics, that is assumed to occur in a particular study area,
following a specified path and timing sequence.
TRANSPOSED--A hypohurricane based on the storm transposition principle, assumed to have wind patterns and other characteristics basically comparable to a specified hurricane of record, but transposed to follow a new path to serve as a basis for computing a hurricane surge hydrograph that would be expected at a selected point. Moderate adjustments in timing or rate of forward movement may also be made, if these are compatible with meteorological considerations and study objectives.
HYPOHURRICANE BASED ON GENERALIZED PARAMETERS--Hypohurricane estimates based on various logical combinations of hurricane characteristics used in estimating hurricane surge magnitudes corresponding to a range of probabilities and potentialities. The STANDARD PROJECT HURRICANE is most commonly used for this purpose, but estimates corresponding to more severe or less severe assumptions are important in some project investigations.
STANDARD PROJECT HURRICANE (SPH)--A hypothetical hurricane intended to represent the most severe combination of hurricane parameters that is reasonably characteristic of a specified region, excluding extremely rare combinations. It is further assumed that the SPH would approach a given project site from such direction, and at such rate of movement, to produce the highest HURRICANE SURGE HYDROGRAPH, considering pertinent hydraulic characteristics of the area. Based on this concept, and on extensive meteorological studies and probability analyses, a tabulation of "Standard Project Hurricane Index Characteristics" mutually agreed upon by representatives of the U. S. Weather Service and the Corps of Engineers, is available.
PROBABLE MAXIMUM HURRICANE--A hypohurricane that might result from the most severe combination of hurricane parameters that is considered reasonably possible in the region involved, if the hurricane should approach the point under study along a critical path and at optimum rate of movement. This estimate is substantially more severe than the SPH criteria.
DESIGN HURRICANE--A representation of a hurricane with specified characteristics that would produce HURRICANE SURGE HYDROGRAPHS and coincident wave effects at various key locations along a proposed project alinement. It governs the project design after economics and other factors have been duly considered. The design hurricane may be more or less severe than the SPH, depending on economics, risk, and local considerations.
A loosely-used synonym of glacial epoch, or time of extensive glacial activity; specifically of the latest period of widespread continental glaciers, the PLEISTOCENE Epoch.
The floating vertical cliff forming the seaward edge of an ICE SHELF or other glacier that enters the sea.
A extensive sheet of ice which is attached to the land along one side but most of which is afloat and bounded on the seaward side by a steep cliff (ICE FRONT) rising 2 tp 50+ m above sea level. Common along polar coasts (Antarctica, Greenland), and generally of great breadth and sometimes extending tens or hundreds of km seaward from the continental coastline.
A GROIN constructed such that sand cannot pass through the structure (but sand may still move over or around it).
Wave moving landward.
INDIAN SPRING LOW WATER
The approximate level of the mean of lower low waters at spring tides, used principally in the Indian Ocean and
along the east coast of Asia. Also INDIAN TIDE PLANE.
INDIAN TIDE PLANE
The datum of INDIAN SPRING LOW WATER.
Long waves with periods of 30 seconds to several minutes.
Waters landward of the baseline (COASTLINE) from which the marginal seas are measured and over which
complete sovereignty is exercised. Also known as “internal waters.”
(1) A short, narrow waterway connecting a bay, lagoon, or similar body of water with a large parent body of water.
(2) An arm of the sea (or other body of water) that is long compared to its width and may extend a considerable distance
inland. See also TIDAL INLET.
Generally, the deepest region of an inlet channel.
In beach terminology, the zone of variable width extending from the LOW WATER LINE through the BREAKER ZONE. Also SHOREFACE. (See Figure A-1)
Any current in or landward of the BREAKER ZONE.
The zone surrounding an island extending from the LOW WATER LINE to the depth (usually about 183 m;
100 fathoms) where there is a marked or rather steep descent toward the great depths.
Waves that occur within a fluid whose density changes with depth, either abruptly at a sharp surface of discontinuity (an interface), or gradually. Their amplitude is greatest at the density discontinuity or, in the case of a gradual density change, somewhere in the interior of the fluid and not at the free upper surface where the surface waves have their maximum amplitude.
The zone between the high and low water tides.
Waves with random wave periods (and in practice, also heights), which are typical for natural wind-induced waves.
A wave with fluid particles that do not revolve around an axis through their centers, although the particles themselves may travel in circular or nearly circular orbits. Irrotational waves may be PROGRESSIVE, STANDING, OSCILLATORY, or TRANSLATORY. For example, the Airy, Stokes, cnoidal, and solitary wave theories describe irrotational waves. Compare TROCHOIDAL WAVE.
A contour line connecting points of equal water depths on a CHART.
Line connecting points on the seabed with an equal depth of sediment.
See HURRICANE WIND PATTERN.
A narrow strip of land, bordered on both sides by water, that connects two larger bodies of land.
To place (a pile, slab, or pipe) in the ground by means of a jet of water acting at the lower end.
(1) (United States usage) On open seacoasts, a structure extending into a body of water, which is designed to prevent shoaling of a channel by littoral materials and to direct and confine the stream or tidal flow. Jetties are built at the mouths of rivers or tidal inlets to help deepen and stabilize a channel. (2) (British usage) WHARF or PIER. See TRAINING WALL.
The probability of two (or more) things occurring together.
JOINT PROBABILITY DENSITY
Function specifying the joint distribution of two (or more) variables.
JOINT RETURN PERIOD
Average period of time between occurrences of a given joint probability event.
Wave spectrum typical of growing deep water waves developed from field experiments and measurements of waves and wave spectra in the Joint North Sea Wave Peoject
Wind caused by cold air flowing down slopes due to gravitational acceleration.
A cay, esp. one of the low, insular banks of sand, coral, and limestone off the southern coast of Florida.
The dynamic viscosity divided by the fluid density.
KINETIC ENERGY (OF WAVES)
In a progressive oscillatory wave, a summation of the energy of motion of the particles within the wave.
A submerged elevation of rounded shape rising less than 1000 meters from the ocean floor and of limited extent across the summit. Compare SEAMOUNT.
The unit of speed used in navigation equal to 1 nautical mile (6,076.115 ft or 1,852 m) per hour.
LAGGING OF TIDE
The periodic retardation in the time of occurrence of high and low water due to changes in the relative positions of the moon and sun.
A shallow body of water, like a pond or sound, partly or completely separated from the sea by a BARRIER
ISLAND or REEF. Sometimes connected to the sea via an INLET. (See Figure IV-1-6.)
Slow, smooth flow, with each drop of water traveling a smooth path parallel to its neighboring drops. Laminar flow is characteristic of low velocities, and particles of sediment in the flow zones are moved by rolling or SALTATION.
A light wind blowing from the land to the sea, caused by unequal cooling of land and water masses.
The combination of a land breeze and a sea breeze as a diurnal phenomenon.
Enclosed, or nearly enclosed, by land--thus protected from the sea, as a bay or a harbor.
A conspicuous object, natural or artificial, located near or on land, which aids in fixing the position of an observer.
A line, wire, or cord used in sounding (to obtain water depth). It is weighted at one end with a plummet (sounding lead). Also SOUNDING LINE.
A rocky formation forming a ridge or REEF, especially one underwater or near shore
(1) Shelter, or the part or side sheltered or turned away from the wind or waves. (2) (Chiefly nautical) The quarter or region toward which the wind blows.
The direction toward which the wind is blowing; the direction toward which waves are traveling.
LENGTH OF WAVE
The horizontal distance between similar points on two successive waves measured perpendicularly to the crest.
(1) A ridge or EMBANKMENT of sand and silt, built up by a stream on its flood plain along both banks of its channel. (2) A large DIKE or artificial EMBANKMENT, often having an access road along the top, which is designed as part of a system to protect land from floods.
A wind with velocity from 4 to 6 KNOTS.
LIMIT OF BACKRUSH (LIMIT OF BACKWASH)
See BACKRUSH, BACKWASH.
Of or pertaining to a shore, especially of the sea. Often used as a general term for the coastal zone influenced by wave action, or, more specifically, the shore zone between the high and low water marks.
A reach of the coast that is isolated sedimentologically from adjacent coastal reaches and that features its own sources and sinks. Isolation is typically caused by protruding headlands, submarine canyons, inlets, and some river mouths that prevent littoral sediment from one cell to pass into the next. Cells may range in size from a multi-hundred meter POCKET BEACH in a rocky coast to a BARRIER ISLAND many tens of kilometers long.
See CURRENT, LITTORAL.
Deposits of littoral drift.
LITTORAL DRIFT, LITTORAL TRANSPORT
The movement of beach material in the littoral zone by waves and currents. Includes movement parallel (long shore drift) and sometimes also perpendicular (cross-shore transport) to the shore.
LITTORAL TRANSPORT RATE
Rate of transport of sedimentary material parallel or perpendicular to the shore in the littoral zone. Usually expressed in cubic meters (cubic yards) per year. Commonly synonymous with LONGSHORE TRANSPORT RATE.
In beach terminology, an indefinite zone extending seaward from the shoreline to just beyond the breaker zone.
The quantity of sediment transported by a current. It includes the suspended load of small particles and the BED LOAD of large particles that move along the bottom.
Waves with periods above about 30 seconds; can be generated by wave groups breaking in the surf zone. See also INFRAGRAVITY WAVES.
Parallel to and near the shoreline; ALONGSHORE.
A sand ridge or ridges, running roughly parallel to the shoreline and extending along the shore outside the trough, that may be exposed at low tide or may occur below the water level in the offshore.
See CURRENT, LONGSHORE.
Movement of (beach) sediments approximately parallel to the coastline.
LONGSHORE TRANSPORT RATE
See LITTORAL TRANSPORT RATE.
An elongate DEPRESSION or series of depressions extending along the lower BEACH or in the offshore zone inside the BREAKERS.
That part of a STANDING WAVE where the vertical motion is greatest and the horizontal velocities are least.
Loops (sometimes called ANTINODES) are associated with CLAPOTIS and with SEICHE action resulting from wave
reflections. Compare NODE.
LOW TIDE (LOW WATER, LW)
The minimum elevation reached by each falling tide. See TIDE. (See Figure II-5-16.)
LOW TIDE TERRACE
A flat zone of the beach near the low water level.
LOW WATER (LW)
The minimum height reached by each falling tide. Nontechnically, also called LOW TIDE.
LOW WATER DATUM
An approximation to the plane of mean low water that has been adopted as a standard reference plane. See also
DATUM, PLANE and CHART DATUM.
LOW WATER LINE
The line where the established LOW WATER DATUM intersects the shore. The plane of reference that constitutes the LOW WATER DATUM differs in different regions.
LOW WATER OF ORDINARY SPRING TIDES (LWOST)
A tidal datum appearing in some British publications, based on low water of ordinary spring tides.
LOWER HIGH WATER (LHW)
The lower of the two high waters of any tidal day. (See Figure II-5-16.)
LOWER LOW WATER DATUM
An approximation to the plane of MEAN LOWER LOW WATER that has been adopted as a standard reference plane for a limited area and is retained for an indefinite period regardless of the fact that it may differ slightly from a better determination of MEAN LOWER LOW WATER from a subsequent series of observations.
LOWER LOW WATER (LLW)
The lower of the two low waters of any tidal day. The single low water occurring daily during periods when the
tide is diurnal is considered to be a lower low water. (See Figure II-5-16.)
LOWEST ASTRONOMICAL TIDE (LAT)
The lowest tide level which can be predicted to occur under average meteorological conditions and any
combination of astronomical conditions. This level may not be reached every year.
The time of rotation of the Earth with respect to the moon, or the interval between two successive upper transits of the moon over the meridian of a place. The mean lunar day is approximately 24.84 solar hours in length, or 1.035 times as great as the mean solar day. Also called TIDAL DAY.
The portion of the tide that can be attributed directly to attraction to the moon.
Higher-than-normal wave generated when waves strike a structure at an oblique angle.
Tidal range greater than 4 m.
The deliberate setting back (moving landward) of the existing line of sea defense in order to obtain engineering or environmental advantages - also referred to as managed landward realignment. Sometimes refers to moving roads and utilities landward in the face of shore retreat.
A tropical tree with interlacing prop roots, confined to low-lying brackish areas.
A zone separating a continent from the deep-sea bottom.
The probability of a single variable in the context of a joint probability analysis.
MARGINAL RETURN PERIOD
The return period of a single variable in the context of a joint probability analysis.
The maritime belt over which a coastal state asserts sovereignty.
A graphic record of the rise and fall of the tide. The record is in the form of a curve in which time is represented by abscissas and the height of the tide by ordinates.
A mark of permanent character close to a survey station, to which it is related by an accurately measured distance and azimuth (or bearing).
An object placed at the site of a station to identify the surveyed location of that station.
(1) A tract of soft, wet land, usually vegetated by reeds, grasses and occasionally small shrubs. (2) Soft, wet area periodically or continuously flooded to a shallow depth, usually characterized by a particular subclass of grasses, cattails and other low plants.
A former salt marsh which has been protected by a DIKE.
A marsh periodically flooded by salt water.
MASS TRANSPORT, SHOREWARD
The movement of water due to wave motion, which carries water through the BREAKER ZONE in the direction of wave propagation. Part of the NEARSHORE CURRENT SYSTEM.
A blanket of brushwood or bamboo, poles, geotextile and reed lashed together to protect a shoreline, embankment or river/sea bed against erosion. Sometimes placed on the sea bed during JETTY construction to prevent stone from settling into soft bottom.
The average DEPTH of the water area between the still water level and the SHOREFACE profile from the waterline to any chosen distance seaward.
MEAN DIAMETER, GEOMETRIC
See GEOMETRIC MEAN DIAMETER.
MEAN HIGH WATER LINE
The intersection of the tidal plane of mean high water with the shore. (Similar definitions apply to mean low water line and mean lower low water line).
MEAN HIGH WATER SPRINGS (MHWS)
The average height of the high water occurring at the time of spring tides.
MEAN HIGH WATER (MHW)
The average height of the high waters over a 19-year period. For shorter periods of observations, corrections are applied to eliminate known variations and reduce the results to the equivalent of a mean 19-year value. All high water heights are included in the average where the type of tide is either semidiurnal or mixed. Only the higher high water heights are included in the average where the type of tide is diurnal. So determined, mean high water in the latter case is the same as mean higher high water.
MEAN HIGHER HIGH WATER (MHHW)
The average height of the higher high waters over a 19-year period. For shorter periods of observation, corrections are applied to eliminate known variations and reduce the result to the equivalent of a mean 19-year value.
MEAN LOW WATER (MLW)
The average height of the low waters over a 19-year period. For shorter periods of observations, corrections are applied to eliminate known variations and reduce the results to the equivalent of a mean 19-year value. All low water heights are included in the average where the type of tide is either semidiurnal or mixed. Only lower low water heights are included in the average where the type of tide is diurnal. So determined, mean low water in the latter case is the same as mean lower low water.
MEAN LOW WATER SPRINGS
The average height of low waters occurring at the time of the spring tides. It is usually derived by taking a plane depressed below the half-tide level by an amount equal to one-half the spring range of tide, necessary corrections being applied to reduce the result to a mean value. This plane is used to a considerable extent for hydrographic work outside of the United States and is the plane of reference for the Pacific approaches to the Panama Canal. Frequently abbreviated to LOW WATER SPRINGS.
MEAN LOWER LOW WATER (MLLW)
The average height of the lower low waters over a 19-year period. For shorter periods of observations, corrections are applied to eliminate known variations and reduce the results to the equivalent of a mean 19-year value. Frequently abbreviated to LOWER LOW WATER.
MEAN RANGE OF TIDE
The difference in height between MEAN HIGH WATER and MEAN LOW WATER.
MEAN RISE OF THE TIDE
The height of MEAN HIGH WATER above the plane of reference or DATUM of chart.
MEAN SEA LEVEL
The average height of the surface of the sea for all stages of the tide over a 19-year period, usually determined from hourly height readings. Not necessarily equal to MEAN TIDE LEVEL. It is also the average water level that would exist in the absence of tides.
The ratio of the MEAN DEPTH to the horizontal distance over which the MEAN DEPTH was determined.
MEAN TIDE LEVEL
A plane midway between MEAN HIGH WATER and MEAN LOW WATER. Not necessarily equal to MEAN SEA LEVEL. Also HALF-TIDE LEVEL.
MEAN WATER LEVEL
The mean surface level as determined by averaging the heights of the water at equal intervals of time, usually at hourly intervals.
MEAN WAVE HEIGHT
The mean of all individual waves in an observation interval of approximately half an hour. In case of a Rayleigh-distribution 63% of the significant wave height.
A single channel having a pattern of successive deviations in alignment which results in a more or less sinusoidal course.
Mechanical plant characterized by the use of some form of bucket to excavate and raise the bottom material Normally, the mechanical dredge deposits material into a barge that transports it to the disposal site, but in some cases, the dredged material can be deposited directly in-water or placed on the bank immediately adjacent to the work area. Mechanical dredges may be classified into two sub-groups by how their buckets are connected to the dredge: (1) wire rope (i.e., clamshell or dragline), and (2) structurally (i.e., a backhoe).
The diameter which marks the division of a given sand sample into two equal parts by weight, one part containing all grains larger than that diameter and the other part containing all grains smaller.
See SAND WAVE.
Tidal range between 2 m and 4 m.
Tidal constituents having their origin in the daily or seasonal variation in weather conditions which may occur with some degree of periodicity.
Tidal range less than 2 m.
A plane midway between the extreme high water and the extreme LOW WATER occurring in any locality.
A shoal formed by ebb and flood tides in the middle of the channel of the LAGOON or estuary end of an inlet.
A naturally occurring, inorganic, crystalline solid that has a definite chemical composition and possesses characteristic physical properties.
See DURATION, MINIMUM.
The least distance in which steady-state wave conditions will develop for a wind of given speed blowing a given
duration of time.
Water vapor suspended in the air in very small drops finer than rain, larger than fog.
Type of tidal current characterized by a conspicious velocity difference between the two floods or two ebbs usually occurring each tidal day.
A type of tide in which the presence of a diurnal wave is conspicuous by a large inequality in either the high or low water heights, with two high waters and two low waters usually occurring each tidal day. In strictness, all tides are mixed, but the name is usually applied without definite limits to the tide intermediate to those predominantly semidiurnal and those predominantly diurnal. (See Figure II-5-16.)
In coastal terminology, a massive land-connected, solid-fill structure of earth (generally revetted), masonry, or large stone, which may serve as a breakwater or pier.
A series of waves generated in a laboratory, each of which has the same length and period.
Like a single stone or block. In coastal structures, the type of construction in which the structure's component parts are bound together to act as one.
An accumulation of earth, stones, etc., deposited by a glacier, usually in the form of a mound, ridge or other
prominence on the terrain.
(1) The mutual interaction and adjustment of the seafloor topography and fluid dynamics involving the motion of sediment. (2) The coupled suite of mutually interdependent hydrodynamic processes, seafloor morphologies, and sequences of change.
Single wave condition producing the same net longshore drift as a given proportion of the annual wave climate.
River/estuary/lake/seabed form and its change with time.
Entrance to an inland water body (e.g., river).
A fluid-to-plastic mixture of finely divided particles of solid material and water.
A level area of fine silt and clay along a shore alternately covered or uncovered by the tide or covered by shallow water.
NATIONAL TIDAL DATUM EPOCH (NTDE)
A period of 19 years adopted by the National Ocean Service as the period over which observations of tides are to be taken and reduced to average values for tidal datums.
A component of a sediment deposit that is unique to a particular source and can be used to identify the source and transport routes to a place of deposition.
The length of a minute of arc, 1/21,600 of an average great circle of the Earth. Generally one minute of latitude is considered equal to one nautical mile. The accepted United States value as of 1 July 1959 is 1,852 meters (6,076.115 feet), approximately 1.15 times as long as the U.S. statute mile of 5,280 feet. Also GEOGRAPHICAL MILE.
Waters that are either tidally-influenced or navigable in fact.
A specific and fixed geographic area within a water body or series of water bodies that has been authorized for
navigation by some group or organization (often a national government).
NEAP HIGH WATER
See NEAP TIDE.
NEAP LOW WATER
See NEAP TIDE.
See NEAP TIDE.
NEAP TIDAL CURRENT
Tidal current of decreased velocity occurring semimonthly as the result of the moon being in quadrature.
Tide of decreased range occurring semimonthly as the result of the moon being in quadrature. The NEAP RANGE of the tide is the average semidiurnal range occurring at the time of neap tides and is most conveniently computed from the harmonic constants. The NEAP RANGE is typically 10 to 30 percent smaller than the mean range where the type of tide is either semidiurnal or mixed and is of no practical significance where the type of tide is DIURNAL. The average height of the high waters of the neap tide is called NEAP HIGH WATER or HIGH WATER NEAPS (MHWN), and the average height of the corresponding LOW WATER is called NEAP LOW WATER or LOW WATER NEAPS (MLWN).
(1) In beach terminology an indefinite zone extending seaward from the SHORELINE well beyond the BREAKER ZONE. (2) The zone which extends from the swash zone to the position marking the start of the offshore zone, typically at water depths of the order of 20 m.
Artificial berm built in shallow water using dredged material. Often, the berm is intended to renourish the adjacent and downdrift shore over time under the influence of waves and currents.
The ocean circulation pattern composed of the NEARSHORE CURRENTS and the COASTAL CURRENTS.
NEARSHORE CURRENT SYSTEM
The current system caused primarily by wave action in and near the breaker zone, and which consists of four parts: the shoreward mass transport of water; longshore currents; seaward return flow, including rip currents; and the longshore movement of the expanding heads of rip currents. See also NEARSHORE CIRCULATION.
(1) The narrow strip of land which connects a peninsula with the mainland, or connects two ridges. (2) The narrow band (rip) of water flowing seaward through the surf. See also RIP CURRENT.
Roughly triangular promontory of land jutting into the sea, often consisting of mobile material, i.e. a beach form.
A set consisting of: (a) stations for which geometric relationships have been determined and which are so related that removal of one station from the set will affect the relationships (distances, directions, coordinates, etc.) between the other stations; and (b) lines connecting the stations to show this interdependence.
The cut made by waves in a shoreline of emergence.
An area in which the predominant direction of the LONGSHORE TRANSPORT changes.
That part of a STANDING WAVE where the vertical motion is least and the horizontal velocities are greatest. Nodes are associated with CLAPOTIS and with SEICHE action resulting from wave reflections. Compare LOOP.
The process of replenishing a beach. It may occur naturally by longshore transport, or be brought about artificially by the deposition of dredged materials or of materials trucked in from upland sites.
Refers to analysis of coastal processes using computational models.
The study of the sea, embracing and indicating all knowledge pertaining to the sea's physical boundaries, the
chemistry and physics of seawater, marine biology, and marine geology.
(1) In beach terminology, the comparatively flat zone of variable width, extending from the SHOREFACE to the edge of the CONTINENTAL SHELF. It is continually submerged. (2) The direction seaward from the shore. (3) The zone beyond the nearshore zone where sediment motion induced by waves alone effectively ceases and where the influence of the sea bed on wave action is small in comparison with the effect of wind. (4) The breaker zone directly seaward of the low tide line. (See Figure A-1)
See BARRIER BEACH.
A BREAKWATER built towards the seaward limit of the littoral zone, parallel (or nearly parallel) to the shore.
(1) Any current in the offshore zone. (2) Any current flowing away from shore.
A wind blowing seaward from the land in the coastal area.
A direction landward from the sea.
A wind blowing landward from the sea in the coastal area.
In wave forecasting, a wind blowing in a direction opposite to the ocean-wave advance; generally, a headwind.
In water waves, the path of a water particle affected by the wave motion. In deepwater waves the orbit is nearly circular, and in shallow-water waves the orbit is nearly elliptical. In general, the orbits are slightly open in the direction of wave motion, giving rise to MASS TRANSPORT. (See Figure II-1-4.)
The flow of water accompanying the orbital movement of the water particles in a wave. Not to be confused with wave-generated LITTORAL CURRENTS. (See Figure II-1-4.)
ORDINARY HIGH WATER MARK (OHWM)
Same as MEAN HIGH WATER LINE.
This expression is not used in a technical sense by the U.S. Coast and Geodetic Survey, but the word "ordinary" when applied to tides, may be taken as the equivalent of the word "mean". Thus "ordinary HIGH WATER LINE" may be assumed to be the same as "mean high water line".
On a wave-refraction diagram, a line drawn perpendicularly to the wave crests. Also called WAVE RAY. (See Figure II-3-4)
(1) A periodic motion backward and forward. (2) Vibration or variance above and below a mean value.
A wave in which each individual particle oscillates about a point with little or no permanent change in mean position. The term is commonly applied to progressive oscillatory waves in which only the form advances, the individual particles moving in closed or nearly closed orbits. Compare WAVE OF TRANSLATION. See also ORBIT.
A surface exposure of bare rock, not covered by soil or vegetation.
A structure extending into a body of water for the purpose of discharging sewage, storm runoff, or cooling water.
EROSION behind or around the land-based end of a GROIN, JETTY, or BREAKWATER or the terminus of a BULKHEAD, REVETMENT, or SEAWALL, usually causing failure of the structure or its function
The water that splashes over the top of a BREAKWATER, SEAWALL, etc.
Passing of water over the top of a structure as a result of wave runup or surge action.
(1) The part of the UPRUSH that runs over the crest of a BERM or structure and does not flow directly back to the ocean or lake. (2) The effect of waves overtopping a COASTAL DEFENSE, often carrying sediment landwards which is then lost to the beach system.
A low wall built along the edge of a structure such as a SEAWALL or QUAY.
The velocity induced by wave motion with which a specific water particle moves within a wave.
A moundlike or flat-topped organic REEF, generally less than 1 km across, frequently forming part of a larger reef complex.
In hydrographic usage, a navigable channel through a bar, REEF, or shoal, or between closely adjacent islands. On the Gulf of Mexico coast, inlets are often known as passes (e.g., Sabine Pass).
The wave period determined by the inverse of the frequency at which the wave energy spectrum reaches its
Beach material usually well-rounded and between about 4 mm to 64 mm diameter. See SOIL CLASSIFICATION.
An elongated body of land nearly surrounded by water and connected to a larger body of land by a neck or isthmus.
A beach or fillet of sand retained above the otherwise normal profile level by a submerged dike.
The process by which water flows through the interstices of a sediment. Specifically, in wave phenomena, the
process by which wave action forces water through the interstices of the bottom sediment and which tends to reduce wave
The average semidiurnal range occurring at the time of the PERIGEAN TIDES and most conveniently computed from the harmonic constants. It is larger than the mean range where the type of tide is either semidiurnal or mixed and is of no practical significance where the type of tide is diurnal.
PERIGEAN TIDAL CURRENTS
Tidal currents of increased velocity occurring monthly as the result of the moon being in perigee (i.e., at the point in its orbit nearest the Earth).
Tides of increased range occurring monthly as the result of the moon being in perigee.
A current caused by the tide-producing forces of the moon and the sun; a part of the same general movement of the sea that is manifested in the vertical rise and fall of the tides. See also CURRENT, FLOOD and CURRENT, EBB.
A current that runs continuously, independent of the tides and temporary causes. Permanent currents include the
freshwater discharge of a river and the currents that form the general circulatory systems of the oceans.
The property of bulk material (sand, crushed rock, soft rock in situ) which permit movement of water through its pores.
A GROIN with openings or voids large enough to permit passage of appreciable quantities of LITTORAL DRIFT through the structure.
The systematic description and classification of rocks.
That branch of geology which treats the scientific study of rocks.
In surface wave motion, a point in the period to which the wave motion has advanced with respect to a given initial reference point.
Variations in the tides or tidal currents associated with changes in the phase of the Moon in relation to the Sun.
Propagation velocity of an individual wave as opposed to the velocity of a wave group.
PHI GRADE SCALE
A logarithmic transformation of the Wentworth grade scale for size classifications of sediment grains based on the negative logarithm to the base 2 of the particle diameter: = -log2d. See SOIL CLASSIFICATION.
The zone extending downward from the ocean surface within which the light is sufficient to sustain photosynthesis. The depth of this layer varies with water clarity, time of year and cloud cover, but is about 100 m in the open ocean. It may be considered the Depth to which all light is filtered out except for about one percent and may be calculated as about two and one-half times the depth of a SECCHI DISK reading.
The science of deducing the physical dimensions of objects from measurements on images (usually photographs) of the objects.
An assemblage of photographs, each of which shows part of a region, put together in such a way that each point in the region appears once and only once in the assemblage, and scale variation is minimized.
Upper surface of an unconfined aquifer (e.g. the top sand layer in a dike) at which the pressure in the groundwater is equal to atmospheric pressure.
A large division of Geology concerned with earth materials, changes of the surface and interior of the earth, and the forces that cause those changes.
Refers to the investigation of coastal or riverine processes using a scaled model.
A structure, usually of open construction, extending out into the water from the shore, to serve as a landing place, recreational facility, etc., rather than to afford coastal protection or affect the movement of water. In the Great Lakes, a term sometimes improperly applied to jetties.
Wave spectrum typical of fully-developed deep water waves.
The level at which the hydrostatic water pressure in an aquifer will stand if it is free to seek equilibrium with the
atmosphere. For artesian wells, this is above the ground surface.
A long, heavy timber or section of concrete or metal that is driven or jetted into the earth or seabed to serve as a
support or protection.
A group of piles.
Erosion of closed flow channels (tunnels) by the passage of water through soil; flow underneath structures, carrying away particles, may endanger the stability of the structure.
Mineral deposits consisting of dense, resistant and often economically valuable minerals which have been
weathered from TERRIGENOUS rocks, transported to the sea and concentrated in marine sediments by wave or current
Surface mines in which valuable mineral grains are extracted from stream bar or beach deposits.
See COASTAL PLAIN.
The outline or shape of a body of water as determined by the still-water line.
A land area (usually extensive) having a relatively level surface raised sharply above adjacent land on at least one side; table land. A similar undersea feature.
An epoch of the Quaternary Period characterized by several glacial ages.
(1) For a plunging wave, the point at which the wave curls over and falls. (2) The final breaking point of the waves just before they rush up on the beach. (See Figure A-1)
A beach, usually small, in a coastal reentrant or between two littoral barriers (often rocky headlands).
(1) The extreme end of a CAPE, or the outer end of any land area protruding into the water, usually less prominent than a CAPE. (2) A low profile shoreline promontory of more or less triangular shape, the top of which extends seaward.
Said of a clastic sediment or rock that consists of particles of many sizes mixed together in an unsystematic manner so that no one size class predominates.
The interstitial pressure of water within a mass of soil or rock.
Percentage of the total volume of a soil sample not occupied by solid particles but by air and water, η = Vv/VT × 100.
A place where vessels may discharge or receive cargo; it may be the entire harbor including its approaches and anchorages, or only the commercial part of a harbor where the QUAYS, WHARVES, facilities for transfer of cargo, docks, and repair shops are situated. Protection may be provided by natural or artificial features.
POTENTIAL ENERGY OF WAVES
In a progressive oscillatory wave, the energy resulting from the elevation or depression of the water surface from the undisturbed level.
See TIDAL PRISM.
The chance that a prescribed event will occur, represented by a number (p) in the range 0 - 1. It can be estimated empirically from the relative frequency (i.e. the number of times the particular event occurs, divided by the total count of all events in the class considered).
Function specifying the distribution of a variable.
PROBABLE MAXIMUM WATER LEVEL
A hypothetical water level (exclusive of wave runup from normal wind-generated waves) that might result from the most severe combination of hydrometeorological, geoseismic, and other geophysical factors and that is considered reasonably possible in the region involved, with each of these factors considered as affecting the locality in a maximum manner.
This level represents the physical response of a body of water to maximum applied phenomena such as hurricanes, moving squall lines, other cyclonic meteorological events, tsunamis, and astronomical tide combined with maximum probable ambient hydrological conditions such as wave setup, rainfall, runoff, and river flow. It is a water level with virtually no risk of being exceeded.
The part of a DELTA that is below the effective depth of wave erosion, lying beyond the delta front and sloping down into the basin into which the delta is advancing.
The intersection of the ground surface with a vertical plane; typically perpendicular to the local shoreline, and may extend from the behind the DUNE line or the top of a bluff to well seaward of the breaker zone. (See Figure A-1)
PROGRESSION (of a beach)
A wave that moves relative to a fixed coordinate system in a fluid. The direction in which it moves is termed the direction of wave propagation.
A high point of land projecting into a body of water; a HEADLAND.
PROPAGATION OF WAVES
The transmission of waves through water.
In laboratory usage, the full-scale structure, concept, or phenomenon used as a basis for constructing a scale model or copy.
Waste of generally small material, in a quarry, left after selection of larger grading.
Any stone processed from a quarry.
(1) The youngest geologic period; includes the present time. (2) The latest period of time in the stratigraphic column, 0 – 2 million years, represented by local accumulations of glacial (PLEISTOCENE) and post-glacial (HOLOCENE) deposits which continue, without change of fauna, from the top of the Pliocene (Tertiary). The quaternary appears to be an artificial division of time to separate pre-human from post-human sedimentation. As thus defined, the quaternary is increasing in duration as man’s ancestry becomes better understood.
QUAY (pronounced KEY)
A stretch of paved bank, or a solid artificial landing place parallel to the navigable waterway, for use in loading and unloading vessels.
Loose, yielding, wet sand which offers no support to heavy objects. The upward flow of the water has a velocity that eliminates contact pressures between the sand grains and causes the sand-water mass to behave like a fluid that yields easily to pressure and tends to suck down heavy objects.
An instrument for determining the distance and direction to an object by measuring the time needed for radio
signals to travel from the instrument to the object and back, and by measuring the angle through which the instrument’s
antenna has traveled.
RADIOACTIVE DATING (RADIOMETRIC DATING)
Calculating an age in years for geologic materials by measuring the presence of a short-life radioactive element (e.g., carbon-14) or a long-life element (e.g., potassium-40/argon-40). The term applies to all methods of age determination based on nuclear decay of naturally-occurring radioactive isotopes. Carbon-14 methods are often used to determine the age of peat or wood found in BARRIER ISLANDS.
RADIUS OF MAXIMUM WINDS
Distance from the eye of a hurricane, where surface and wind velocities are zero, to the place where surface
windspeeds are maximum.
A wave-cut platform, with or without a covering of beach materials, which is now raised above the present sea-
The laboratory simulation of irregular sea states that occur in nature.
RANGE OF TIDE
The difference in height between consecutive high and low waters. The MEAN RANGE is the difference between MEAN HIGH WATER and MEAN LOW WATER. The GREAT DIURNAL RANGE or DIURNAL RANGE is the difference in height between MEAN HIGHER HIGH WATER (MHHW) and MEAN LOWER LOW WATER (MLLW). Where the type of tide is diurnal, the mean range is the same as the diurnal range.
A model probability distribution, commonly used in analysis of waves.
(1) An arm of the ocean extending into the land, e.g., an ESTUARY. (2) A straight section of restricted waterway that is uniform with respect to discharge, slope, and cross-section.
(Geological) A synonym of HOLOCENE. See also QUATERNARY.
(1) A continuing landward movement of the shoreline. (2) A net landward movement of the shoreline over a
The addition of new water to an AQUIFER or to the zone of saturation.
The process of producing, from a tilted or oblique photograph, a photograph from which displacement caused by tilt has been removed.
A spit whose outer end in turned landward by current deflection, by the opposing action of two or more currents, or by WAVE REFRACTION; a HOOK.
Discoloration of surface waters, most frequently in COASTAL ZONES, caused by large concentrations of microorganisms.
An offshore consolidated rock hazard to navigation, with a least depth of about 20 meters (10 fathoms) or less. Often refers to coral FRINGING REEFS in tropical waters.
See BARRIER REEF.
Rubble mound of single-sized stones with a crest at or below sea level which is allowed to be (re)shaped by the waves.
See FRINGING REEF.
The plane to which sounding and tidal data are referred. See DATUM PLANE.
(1) A specified location (in plan elevation) to which measurements are referred. (2) In beach material studies, a specified point within the REFERENCE ZONE.
A place for which tidal constants have previously been determined and which is used as a standard for the comparison of simultaneous observations at a second station. Also, a station for which independent daily predictions are given in the tide or current tables from which corresponding predictions are obtained for other stations by means of differences or factors.
In regard to beach measuring procedure, the part of the FORESHORE subject to wave action (between the Limit of UPRUSH and the Limit of BACKWASH) at mid-tide stage. In areas of great tidal range a more complex definition is needed.
That part of an incident wave that is returned seaward when a wave impinges on a steep beach, barrier, or other reflecting surface.
The process by which the energy of the wave is returned seaward.
REFRACTION (of water waves)
(1) The process by which the direction of a wave moving in shallow water at an angle to the contours is changed: the part of the wave advancing in shallower water moves more slowly than that part still advancing in deeper water, causing the wave crest to bend toward alinement with the underwater contours. (2) The bending of wave crests by currents. (See Figure II-6-11.)
The square root of the ratio of the distance between adjacent orthogonals in deep water to their distance apart in
shallow water at a selected point. When multiplied by the SHOALING FACTOR and a factor for friction and percolation,
this becomes the WAVE HEIGHT COEFFICIENT or the ratio of the refracted wave height at any point to the deepwater
wave height. Also, the square root of the ENERGY COEFFICIENT.
A drawing showing positions of wave crests and/or orthogonals in a given area for a specific deepwater wave period and direction. (See Figure II-6-11.)
Waves with a single height, period, and direction.
An artificial lake, basin or tank in which a large quantity of water can be stored.
RESIDUAL (WATER LEVEL)
The components of water level not attributable to astronomical effects.
The phenomenon of amplification of a free wave or oscillation of a system by a forced wave or oscillation of
exactly equal period. The forced wave may arise from an impressed force upon the system or from a boundary condition.
The amount of time by which corresponding tidal phases grow later day by day (about 50 minutes).
RETROGRESSION (of a beach)
Average period of time between occurrences of a given event.
REVERSING TIDAL CURRENT
A tidal current that flows alternately in approximately opposite directions with a SLACK WATER at each reversal of direction. Currents of this type usually occur in rivers and straits where the direction of flow is more or less restricted to certain channels. When the movement is towards the shore, the current is said to be flooding, and when in the opposite direction it is said to be ebbing.
(1) A facing of stone, concrete, etc., to protect an EMBANKMENT, or shore structure, against erosion by wave
action or currents. (2) A retaining wall. (3) Facing of stone, concrete, etc., built to protect a SCARP, EMBANKMENT or
shore structure against erosion by waves of currents.
The dimensionless ratio of the inertial force to the viscous force in fluid motion,
Re = LV/g
where L is a characteristic length, g (Greek gamma) the kinematic viscosity, and V a characteristic velocity. The Reynolds number is of importance in the theory of hydrodynamic stability and the origin of turbulence.
A long, narrow inlet, with depth gradually diminishing inward. Shorter and shallower than a FJORD.
RIDGE AND RUNNEL
Beach topography consisting of sand bars that have welded to the shore during the recovery stage after a storm. At low tide, water ponds in the runnels and flows seaward through gaps in the ridge (see Figure IV-2-31).
A nearly continuous mound of beach material that has been shaped by wave or other action. Ridges may occur singly or as a series of approximately parallel deposits.
Tiny drainage channels in a beach caused by the flow seaward of water left in the sands of the upper part of the beach after the retreat of the tide or after the dying down of storm waves.
A body of water made rough by waves meeting an opposing current, particularly a tidal current; often found where tidal currents are converging and sinking.
A channel cut by seaward flow of RIP CURRENT, usually crosses a LONGSHORE BAR.
A strong surface current flowing seaward from the shore. It usually appears as a visible band of agitated water and is the return movement of water piled up on the shore by incoming waves and wind. With the seaward movement concentrated in a limited band its velocity is somewhat accentuated. A rip consists of three parts: the FEEDER CURRENTS flowing parallel to the shore inside the breakers; the NECK, where the feeder currents converge and flow through the breakers in a narrow band or "rip"; and the HEAD OF RIP, where the current widens and slackens outside the breaker line. A rip current is often miscalled a rip tide. Also called RIP SURF.
See RIP CURRENT.
Incorrect term for RIP CURRENT.
(1) Pertaining to the banks of a body of water. (2) Of, on or pertaining to the banks of a river.
(1) The ruffling of the surface of water; hence, a little curling wave or undulation. (2) A wave less than 0.05 meter (2 inches) long controlled to a significant degree by both surface tension and gravity. See CAPILLARY WAVE and GRAVITY WAVE.
Undulations produced by fluid movement over sediments. Oscillatory currents produce symmetric ripples whereas a well-defined current direction produces asymmetrical ripples. The crest line of ripples may be straight or sinuous. The characteristic features of ripples depend upon current velocity, particle size, persistence of current direction and whether the fluid is air or water. Sand DUNES may be regarded as a special kind of ‘super’-ripple.
RIPPLES (bed forms)
Small bed forms with wavelengths less than 0.3 m (1 foot) and heights less than 0.03 m (0.1 foot).
A protective layer or facing of quarrystone, usually well graded within wide size limit, randomly placed to prevent erosion, scour, or sloughing of an embankment or bluff; also the stone so used. The quarrystone is placed in a layer at least twice the thickness of the 50 percent size, or 1.25 times the thickness of the largest size stone in the gradation.
Assessment of the total risk due to all possible environmental inputs and all possible mechanisms.
An area of the sea used for anchorage of vessels and transhipment of cargo, usually without the protection from
weather associated with harbors.
Physical and mineralogical decay processes in rock brought about by exposure to climatic conditions either at the present time or in the geological past.
(1) An aggregate of one or more minerals; or a body of undifferentiated mineral matter (e.g., obsidian). The three classes of rocks are: (a) Igneous – crystalline rocks formed from molten material. Examples are granite and basalt. (b) Sedimentary – resulting from the consolidation of loose sediment that has accumulated in layers. Examples are sandstone, shale and limestone. (c) Metamorphic – formed from preexisting rock as a result of burial, heat, and pressure. (2) A rocky mass lying at or near the surface of the water or along a jagged coastline, especially where dangerous to shipping.
An indefinite term, sometimes considered to denote one of a series of long-crested, large waves which roll in on a shore, as after a storm.
ROTARY CURRENT, TIDAL
A tidal current that flows continually with the direction of flow changing through all points of the compass during the tidal period. Rotary currents are usually found offshore where the direction of flow is not restricted by any barriers. The tendency for the rotation in direction has its origin in the deflecting force of the earth’s rotation and, unless modified by local conditions, the change is clockwise in the Northern Hemisphere and counterclockwise in the Southern Hemisphere. The velocity of the current usually varies throughout the tidal cycle, passing through two maxima in approximately opposite directions and two minima with the direction of the current at approximately ninety degrees from the direction at the time of maximum velocity.
(1) Loose angular waterworn stones along a beach. (2) Rough, irregular fragments of broken rock.
A mound of random-shaped and random-placed stones protected with a cover layer of selected stones or specially shaped concrete armor units. (Armor units in a primary cover layer may be placed in an orderly manner or dumped at random.)
The upper and lower levels reached by a wave on a beach or coastal structure, relative to still-water level.
A corrugation or trough formed in the FORESHORE or in the bottom just offshore by waves or tidal currents (see RIDGE and RUNNEL).
Rubble mound with gentle slope around still-water level and steeper slopes above and below.
A bulge in the coastline projecting towards an offshore island or breakwater, but not connected to it as in the case of a TOMBOLO - see also Ness and Cusp. Developed by WAVE REFRACTION and diffraction and long shore drift.
Number of grams of salt per thousand grams of sea water, usually expressed in parts per thousand (symbol: ‰).
Change in salinity with expressed in parts per thousand per foot.
A marsh periodically flooded by salt water (also tidal marsh; sea marsh).
In this circulation type, the density-driven component dominates and two well-mixed layers are separated by a sharp HALOCLINE. The seawater entering the channel appears as a tongue or wedge.
That method of sand movement in a fluid in which individual particles leave the bed by bounding nearly vertically and, because the motion of the fluid is not strong or turbulent enough to retain them in suspension, return to the bed at some distance downstream. The travel path of the particles is a series of hops and bounds.
Sediment particles, often largely composed of quartz, with a diameter of between 0.062 mm and 2 mm, generally classified as fine, medium, coarse or very coarse. Beach sand may sometimes be composed of organic sediments such as calcareous reef debris or shell fragments.
(1) See BAR. (2) In a river, a ridge of sand built to or near the surface by river currents.
See BYPASSING, SAND.
A DUNE formed of sand.
A narrow sand EMBANKMENT, created by an excess of deposition at its seaward terminus, with its distal end (the end away from the point of origin) terminating in open water.
(1) Longshore sand waves are large-scale features that maintain form while migrating along the shore with speeds on the order of kilometers per year. (2) Large-scale asymmetrical bedforms in sandy river beds having high length to height ratios and continuous crestlines.
An almost vertical slope along the beach caused by erosion by wave action. It may vary in height from a few cm to a meter or so, depending on wave action and the nature and composition of the beach. (See Figure A-1) See also ESCARPMENT.
A two-dimensional histogram showing the joint probability density of two variables within a data sample.
Removal of underwater material by waves and currents, especially at the base or toe of a shore structure.
Protection against erosion of the seabed in front of the toe.
(1) A large body of salt water, second in rank to an ocean, more or less landlocked and generally part of, or connected with, an ocean or a larger sea. Examples: Mediterranean Sea; South China Sea. (2) Waves caused by wind at the place and time of observation. (3) State of the ocean or lake surface, in regard to waves.
A light wind blowing from the sea toward the land caused by unequal heating of land and water masses.
(1) A change wrought by the sea. (2) A marked transformation.
A cliff situated at the seaward edge of the coast.
Members of marine seed plants that grow chiefly on sand or sand-mud bottom. They are most abundant in water less than 9 m deep. The common types are: Eel grass (Zostera), Turtle grass (Thallasia), and Manatee grass (Syringodium).
See MEAN SEA LEVEL.
SEA LEVEL RISE
The long-term trend in MEAN SEA LEVEL.
A dangerous longshore current; a rip current caused by return flow; loosely, the submerged channel or inlet through a bar caused by those currents.
Description of the sea surface with regard to wave action. Also called state of sea.
The coast adjacent to the sea or ocean.
An elevation rising more than 1000 meters above the ocean floor, and of limited extent across the summit.
Waves caused by wind at the place and time of observation.
(1) (Law) All ground between the ordinary high-water and low-water mark. (2) The shore of the sea or ocean, often used in a general sense (e.g., to visit the seashore).
(1) A structure, often concrete or stone, built along a portion of a coast to prevent erosion and other damage by wave action. Often it retains earth against its shoreward face. (2) A structure separating land and water areas to alleviate the risk of flooding by the sea. Generally shore-parallel, although some reclamation SEAWALLS may include lengths that are normal or oblique to the (original) shoreline. A SEAWALL is typically more massive and capable of resisting greater wave forces than a BULKHEAD.
Visibility disk (white and black, 30 cm diameter) used to measure the transparency of the water
(1) Loose, fragments of rocks, minerals or organic material which are transported from their source for varying distances and deposited by air, wind, ice and water. Other sediments are precipitated from the overlying water or form chemically, in place. Sediment includes all the unconsolidated materials on the sea floor. (2) The fine grained material deposited by water or wind.
(See LITTORAL CELL)
Point or area at which beach material is irretrievably lost from a coastal cell, such as an estuary, or a deep channel in the seabed.
Point or area on a coast from which beach material is supplied, such as an eroding cliff, or river mouth.
The main agencies by which sedimentary materials are moved are: gravity (gravity transport); running water (rivers and streams); ice (glaciers); wind; the sea (currents and LONGSHORE DRIFT). Running water and wind are the most widespread transporting agents. In both cases, three mechanisms operate, although the particle size of the transported material involved is very different, owing to the differences in density and viscosity of air and water. The three processes are: rolling or traction, in which the particle moves along the bed but is too heavy to be lifted from it; SALTATION; and suspension, in which particles remain permanently above the bed, sustained there by the turbulent flow of the air or water.
SEDIMENT TRANSPORT PATHS
The routes along which net sediment movement occurs.
The movement of water through small cracks, pores, interstices, out of a body of surface of subsurface water. The loss of water by infiltration from a canal, reservoir or other body of water or from a field. It is generally expressed as flow volume per unit of time.
(1) A standing wave oscillation of an enclosed waterbodythat continues, pendulum fashion, after the cessation of the originating force, which may have been either seismic or atmospheric. (2) An oscillation of a fluid body in response to a disturbing force having the same frequency as the natural frequency of the fluid system. Tides are now considered to be seiches induced primarily by the periodic forces caused by the Sun and Moon. (3) In the Great Lakes area, any sudden rise in the water of a harbor or a lake whether or not it is oscillatory (although inaccurate in a strict sense, this usage is well established in the Great Lakes area).
The return of part of the energy of seismic waves to the earth’s surface after the waves bounce off an acoustic
boundary (typically rock or material of different density).
The bending of seismic waves as they pass from one material to another.
SEISMIC SEA WAVE
A process occurring during sediment transport that tends to separate particles according to their size, density, and shape. A well-sorted distribution contains a limited range of grain sizes and usually indicates that the depositional environment contains a narrow range of sediment sizes or a narrow band of depositional energy. A poorly-sorted distribution contains a wide range of grain sizes indicating multiple sources of sediment or a wide range of deposition energies.
A BEACH that has either natural or engineered sand retention and that can be stable through the continued supply of natural sediment sources, without any mechanical nourishment over a long period. Subsets include:
Natural or Geomorphically Self-sustaining Beaches: self-sustaining naturally without the construction of retaining structures and with no continued mechanical sand nourishment.
Anthropogenically Self-sustaining Beaches: self-sustaining by the construction of retaining structure(s) with or without initial beach fill but with no continued mechanical sand nourishment.
Having a period or cycle of approximately one-half of a tidal day (12.4 hours). The predominating type of tide throughout the world is semidiurnal, with two high waters and two low waters each tidal day. The tidal current is said to be semidiurnal when there are two flood and two ebb periods each day.
The response of an instrument or organism to stimuli from a distant source.
A required open space, specified in shoreline master programs, measured horizontally upland from an perpendicular to the ordinary high water mark.
Superelevation of the water surface over normal surge elevation due to onshore mass transport of the water by wave action alone.
See WIND SETUP.
(1) Commonly, water of such a depth that surface waves are noticeably affected by bottom topography. It is customary to consider water of depths less than one-half the surface wavelength as shallow water. See TRANSITIONAL ZONE and DEEP WATER. (2) More strictly, in hydrodynamics with regard to progressive gravity waves, water in which the depth is less than 1/25 the wavelength.
SHALLOW WATER WAVE
A PROGRESSIVE WAVE which is in water less than 1/25 the wave length in depth.
Instabilities of the surf zone longshore current commonly found on beaches with barred depth profiles. These instabilities are vertical motions with little surface elevation expression. Conservation of vorticity is the restoring mechanism.
See SHEAR INSTABILITIES
The removal of a thin layer of surface material, usually topsoil, by a flowing sheet of water.
Sediment grains under high sheer stress moving as a layer that extends from the bed surface to some distance below (on the order of a few cm). Grains are transported in the direction of fluid flow.
See PILE, SHEET.
A sheet on which field control and hydrographic data such as soundings, depth curves, and regions surveyed with a wire drag are plotted before the production of a final chart.
See CONTINENTAL SHELF.
See INSULAR SHELF.
(1) Loosely and commonly, any beach material coarser than ordinary gravel, especially any having flat or flattish pebbles. (2) Strictly and accurately, beach material of smooth, well-rounded pebbles that are roughly the same size. The spaces between pebbles are not filled with finer materials. Shingle often gives out a musical sound when stepped on. The term is more widely used in Great Britain than in the United States.
(1) (noun) A detached area of any material except rock or coral. The depths over it are a danger to surface navigation. Similar continental or insular shelf features of greater depths are usually termed BANKS. (2) (verb) To become shallow gradually. (3) To cause to become shallow. (4) To proceed from a greater to a lesser depth of water.
Decrease in water depth. The transformation of wave profile as they propagate inshore.
The ratio of the height of a wave in water of any depth to its height in deep water with the effects of refraction,
friction, and percolation eliminated. Sometimes SHOALING FACTOR or DEPTH FACTOR. See also ENERGY
COEFFICIENT and REFRACTION COEFFICIENT.
See SHOALING COEFFICIENT.
The narrow strip of land in immediate contact with the sea, including the zone between high and low water lines. A shore of unconsolidated material is usually called a BEACH. (See Figure A-1). Also used in a general sense to mean the coastal area (e.g., to live at the shore). Also sometimes known as the LITTORAL.
A line at right-angles to the contours in the surf zone.
A terrace made along a COAST by the action of waves and shore currents; it may become dry land by the uplifting of the shore or the lowering of the water. Also known as shore platform or wave-cut platform.
The narrow zone seaward from the low tide SHORELINE, covered by water, over which the beach sands and
gravels actively oscillate with changing wave conditions. See INSHORE (ZONE). ( See Figure A-1)
The intersection of a specified plane of water with the shore or beach (e.g., the high water shoreline would be the intersection of the plane of mean high water with the shore or beach). The line delineating the shoreline on National Ocean Service nautical charts and surveys approximates the mean high water line (United States).
The development of strategic, long-term and sustainable coastal defense and land-use policy within a sediment cell.
A wave, the crest length of which is of the same order of magnitude as the wave length. A system of short-crested waves has the appearance of hills being separated by troughs.
A statistical term relating to the one-third highest waves of a given wave group and defined by the average of their heights and periods. The composition of the higher waves depends upon the extent to which the lower waves are considered. Experience indicates that a careful observer who attempts to establish the character of the higher waves will record values which approximately fit the definition of the significant wave.
SIGNIFICANT WAVE HEIGHT
The average height of the one-third highest waves of a given wave group. Note that the composition of the highest waves depends upon the extent to which the lower waves are considered. In wave record analysis, the average height of the highest one-third of a selected number of waves, this number being determined by dividing the time of record by the significant period. Also CHARACTERISTIC WAVE HEIGHT.
SIGNIFICANT WAVE PERIOD
An arbitrary period generally taken as the period of the one-third highest waves within a given group. Note that the composition of the highest waves depends upon the extent to which the lower waves are considered. In wave record analysis, this is determined as the average period of the most frequently recurring of the larger well-defined waves in the record under study.
(1) A submerged structure across a river to control the water level upstream. (2) The crest of a spillway.
Sediment particles with a grain size between 0.004 mm and 0.062 mm, i.e. coarser than clay particles but finer than sand. See SOIL CLASSIFICATION.
An oscillatory wave having the form of a sinusoid.
SLACK TIDE (SLACK WATER)
The state of a tidal current when its velocity is near zero, especially the moment when a reversing current changes direction and its velocity is zero. Sometimes considered the intermediate period between ebb and flood currents during which the velocity of the currents is less than 0.05 meter per second (0.1 knot). See STAND OF TIDE.
In mass wasting, movement of a descending mass along a plane approximately parallel to the slope of the surface.
A berthing space between two piers.
The steep, downwind slope of a DUNE; formed from loose, cascading sand that generally keeps the slope at the ANGLE OF REPOSE (about 34 deg.).
The degree of inclination to the horizontal. Usually expressed as a ratio, such as 1:25, indicating one unit rise in 25 units of horizontal distance; or in a decimal fraction (0.04). Also called GRADIENT.
A small muddy marshland or tidal waterway which usually connects other tidal areas. See BAYOU.
A structure containing a gate to control the flow of water from one area to another.
In mass wasting, movement along a curved surface in which the upper part moves vertically downward while the lower part moves outward.
Usually refers to beaches (natural or designed) but may also relate to energy-absorbing beach-control structures, including those constructed of rock, where these are used to control or redirect coastal processes rather than opposing or preventing them.
A layer of weathered, unconsolidated material on top of bed rock; in geologic usage, usually defined as containing organic matter and being capable of supporting plant growth.
SOIL CLASSIFICATION (size)
An arbitrary division of a continuous scale of grain sizes such that each scale unit or grade may serve as a convenient class interval for conducting the analysis or for expressing the results of an analysis. There are many classifications used (see Table III-1-2).
A wave consisting of a single elevation (above the original water surface), whose height is not necessarily small
compared to the depth, and neither followed nor preceded by another elevation or depression of the water surfaces.
Process of selection and separation of sediment grains according to their grain size (or grain shape or specific
A coefficient used in describing the distribution of grain sizes in a sample of unconsolidated material. It is defined as So = Q1/Q3 , where Q1 is the diameter (in millimeters) which has 75 percent of the cumulative size-frequency (by weight) distribution smaller than itself and 25 percent larger than itself, and Q3 is that diameter having 25 percent smaller and 75 percent larger than itself.
(1) (noun) a relatively long arm of the sea or ocean forming a channel between an island and a mainland or connecting two larger bodies, as a sea and the ocean, or two parts of the same body; usually wider and more extensive than a STRAIT (e.g., Long Island Sound). (2) (verb) To measure the depth of the water.
A measured depth of water. On hydrographic CHARTS the soundings are adjusted to a specific plane of reference (SOUNDING DATUM).
The plane to which soundings are referred. See also CHART DATUM.
A line, wire, or cord used in sounding, which is weighted at one end with a plummet (sounding lead). Also LEAD LINE.
The ratio of the weight of unit volume of any material to the weight of unit volume of water at 4 deg C, Gs = γs/γw.
Typical values of Gs for soil solids are 2.65 to 2.72.
Linguoid, bar-like feature formed by ebb tidal current flow over a low area of an ebb shield.
A structure over or through a dam for discharging flood flows.
A small point of land or a narrow shoal projecting into a body of water from the shore. (See Figure IV-1-6.)
Overburden or other waste material removed in mining, dredging, and quarrying.
Artificial formation created by the deposit of dredged materials on the seabed.
The average SEMIDIURNAL range occurring at the time of SPRING TIDES and most conveniently computed from the harmonic constants. It is larger than the MEAN RANGE where the type of tide is either SEMIDIURNAL or MIXED, and is of no practical significance where the type of tide is DIURNAL.
SPRING TIDAL CURRENTS
Tidal currents of increased velocity occurring semi-monthly as the result of the moon being new or full.
A tide that occurs at or near the time of new or full moon (SYZYGY) and which rises highest and falls lowest from the mean sea level.
An isolated, pillar-like rocky island isolated from a nearby headland by wave erosion; a needle or chimney rock.
STAND OF TIDE
A interval at high or low water when there is no sensible change in the height of the tide. The water level is stationary at high and low water for only an instant, but the change in level near these times is so slow that it is not usually perceptible. See SLACK TIDE.
STANDARD PROJECT HURRICANE
See HYPOTHETICAL HURRICANE.
A type of wave in which the surface of the water oscillates vertically between fixed points, called nodes, without progression. The points of maximum vertical rise and fall are called antinodes or loops. At the nodes, the underlying water particles exhibit no vertical motion, but maximum horizontal motion. At the antinodes, the underlying water particles have no horizontal motion, but maximum vertical motion. They may be the result of two equal progressive wave trains traveling through each other in opposite directions. Sometimes called CLAPOTIS or STATIONARY WAVE.
A point on the ground whose horizontal or vertical location is used as a basis for obtaining locations of other points.
A wave of essentially stable form which does not move with respect to a selected reference point; a fixed swelling. Sometimes called STANDING WAVE.
The nearly horizontal section which more or less divides the BEACH from the SHOREFACE.
STILL-WATER LEVEL (SWL)
The surface of the water if all wave and wind action were to cease. In deep water this level approximates the midpoint of the wave height. In shallow water it is nearer to the trough than the crest. Also called the UNDISTURBED WATER LEVEL.
Having random variation in statistics.
Sand piled on a beach foreshore to nourish downdrift beaches by natural littoral currents or forces. See FEEDER BEACH.
Quarried or artificially-broken rock for use in construction, either as aggregate or cut into shaped blocks as
Stone heavy enough to require handling individual pieces by mechanical means, generally weighing 900 kg (1 ton) and up.
A rise above normal water level on the open coast due to the action of wind stress on the water surface. Storm surge resulting from a hurricane also includes that rise in level due to atmospheric pressure reduction as well as that due to wind stress. See WIND SETUP.
See STORM SURGE.
A relatively narrow waterway between two larger bodies of water (e.g., Strait of Gibraltar). See also SOUND.
(1) The shore or beach of the ocean or a large lake. The land bordering any large body of water, especially a sea or an arm of the ocean. (2) WHARF, QUAY, or roadway along a water body, esp. in a city, sometimes known as a bund.
A prograded shore built seawards by waves and currents.
A wave-cut platform; an elevated wave-cut terrace
The running aground of a ship upon a STRAND, ROCK, or bottom so that it is fast for a time.
An accumulation of debris (e.g. seaweed, driftwood and litter) cast up onto a beach, and lying along the limit of
wave up rush. A shoreline above the present water level
(1) A course of water flowing along a bed in the Earth. (2) A current in the sea formed by wind action, water
density differences, etc.; e.g. the Gulf Stream. See also CURRENT, STREAM.
A narrow, deep and swift ocean current, such as the Gulf Stream. Opposite of DRIFT CURRENT.
The branch of geology concerned with the internal structure of bed rock and the shapes, arrangement, and
interrelationships of rock units.
Situated or occurring on or adjacent to the surface of the earth, usually meaning above the water surface.
That part of the beach which is uncovered by water (e.g. at low tide sometimes referred to as drying beach).
Existing, formed, or taking place under water; submerged
The part or the beach (where it exists) which extends from low water out to the approximate limit of storm erosion. The latter is typically located at a maximum water depth of 8 to 10 meters and is often identifiable on surveys by a break in the slope of the bed.
Flow for which the Froude number is less than unity; surface disturbances can travel upstream.
Elongate region in which the sea floor slides beneath a continent or island arc.
V-shaped valleys that run across the CONTINENTAL SHELF and down the CONTINENTAL SLOPE.
A COAST in which formerly dry land has been recently drowned, either by land subsidence or a rise in sea level.
A tide or current station at which a short series of observations has been obtained, which is to be reduced by comparison with simultaneous observations at another station having well-determined tidal or current constants.
Sinking or downwarping of a part of the earth’s surface.
SUBMERGED LANDS ACT
United States federal legislation that granted to the coastal states federal rights to natural resources within 3 nautical miles (up to 9 miles for Texas and the Gulf coast of Florida) of the COASTLINE).
Below the low-water datum; thus permanently submerged.
Flow for which the Froude number is greater than unity; surface disturbances will not travel upstream.
(1) Collective term for BREAKERS. (2) The wave activity in the area between the shoreline and the outermost limit of breakers. (3) In literature, the term surf usually refers to the breaking waves on shore and on reefs when accompanied by a roaring noise caused by the larger waves breaking.
Irregular oscillations of the nearshore water level with periods on the order of several minutes.
The zone of wave action extending from the water line (which varies with tide, surge, set-up, etc.) out to the most seaward point of the zone (breaker zone) at which waves approaching the coastline commence breaking, typically in water depths of between 5 to 10 meters.
SURFACE GRAVITY WAVE (PROGRESSIVE)
(1) this is the term which applies to the WIND WAVES and SWELL of lakes and oceans, also called SURFACE
WATER WAVE, SURFACE WAVE or DEEP WATER WAVE, (2) a progressive GRAVITY WAVE in which the
disturbance is confined to the upper limits of a body of water. Strictly speaking this term applies to those progressive
GRAVITY WAVES whose celerity depends only upon the wave length.
SURFACE WATER WAVE
See SURFACE GRAVITY WAVE (PROGRESSIVE).
(1) The name applied to wave motion with a period intermediate between that of the ordinary wind wave and that of the tide, say from ½ to 60 min. It is low height, usually less than 0.9 m (3 ft). See also SEICHE. (2) In fluid flow, long interval variations in velocity and pressure, not necessarily periodic, perhaps even transient in nature. (3) see STORM SURGE.
A survey that provides coordinates (horizontal or vertical) of points to which supplementary surveys are adjusted.
A survey that has as its principal purpose the determination of geometric and dynamic characteristics of bodies of water.
A survey in which monuments are placed at points that have been determined photogrammetrically.
A survey which has, for its major purpose, the determination of the configuration (relief) of the surface of the land and the location of natural and artificial objects thereon.
(1) The material moving in suspension in a fluid, kept up by the upward components of the turbulent currents or by colloidal suspension. (2) The material collected in or computed from samples collected with a SUSPENDED LOAD SAMPLER. Where it is necessary to distinguish between the two meanings given above, the first one may be called the "true suspended load."
SUSPENDED LOAD SAMPLER
A sampler which attempts to secure a sample of the water with its sediment load without separating the sediment
from the water.
A beach area that is now and will continue to receive sufficient sediment input over a long period (years or decades) to remain stable. Such sediment input can be through either natural supplies of sediment or various forms of mechanical beach nourishment (placement by hydraulic dredge, land haul of material, nearshore deposition, etc.)
The depression between two beach ridges.
The rush of water up onto the beach face following the breaking of a wave. Also UPRUSH, RUNUP.
Low broad sandy bars formed by sediment in the surf and swash zones, separated by linear depressions, or RUNNELS, running parallel to the shore. Sand bodies that form and migrate across ebb-tidal shoals because of currents generated by breaking waves.
(1) On the open shore, a channel cut by flowing water in its return to the present body (e.g., a rip channel). (2) A secondary channel passing through or shoreward of an inlet or river bar.
The thin wavy line of fine sand, mica scales, bits of seaweed, etc., left by the uprush when it recedes from its upward limit of movement on the beach face.
Sand sheet located between the main ebb channel of a coastal inlet and an adjacent barrier island.
The zone of wave action on the beach, which moves as water levels vary, extending from the limit of run-down to the limit of run-up.
Wind-generated waves that have traveled out of their generating area. Swell characteristically exhibits a more regular and longer period and has flatter crests than waves within their fetch (SEAS).
A chart showing the distribution of meteorological conditions over a given area at a given time. Popularly called a weather map.
The two points in the Moon's orbit when the Moon is in conjunction or opposition to the Sun relative to the Earth; time of new or full Moon in the cycle of phases.
A GROIN built in the shape of a letter “T” with the trunk section connected to land.
Forces generated from within the earth that result in uplift, movement, or deformation of part of the earth’s crust.
The study of the major structural features of the Earth’s crust or the broad structure of a region.
A GROIN, often at the end of a littoral cell or at the UPDRIFT side of an inlet, intended to prevent sediment
passage into the channel beyond.
A horizontal or nearly horizontal natural or artificial topographic feature interrupting a steeper slope, sometimes
occurring in a series.
Literally ‘land-formed’ sediment that has found its way to the sea floor. The term is applied (a) to sediments formed and deposited on land (e.g., soils, sand DUNES), and (b) to material derived from the land when mixed in with purely marine material (e.g., sand or clay in a shelly limestone).
The offshore belt in which a coastal state has exclusive jurisdiction. The territorial sea may not extend more than 12 NAUTICAL MILES from the COASTLINE.
Concrete armor unit with four stubby legs, used on breakwaters and seawalls to dissipate wave energy.
In hydraulics, the line joining the deepest points of an inlet or stream channel. Often serving as the boundary
between two states.
THRESHOLD OF MOTION
The point at which the forces imposed on a sediment particle overcome its inertia and it starts to move.
The maximum orbital velocity at which the sediment on the BED begins to move as waves approach shallow water.
A creek draining back-barrier areas with a current generated by the rise and fall of the tide.
See CURRENT, TIDAL.
See CHART DATUM and DATUM PLANE.
The time of the rotation of the Earth with respect to the Moon, or the interval between two successive upper transits of the Moon over the meridian of a place, approximately 24.84 solar hours (24 hours and 50 minutes) or 1.035 times the mean solar day. (See Figure II-5-16.) Also called lunar day.
(1) Marshy or muddy areas covered and uncovered by the rise and fall of the tide. A TIDAL MARSH. (2) Marshy or muddy areas of the seabed which are covered and uncovered by the rise and fall of tidal water.
(1) A natural inlet maintained by tidal flow. (2) Loosely, any inlet in which the tide ebbs and flows. Also TIDAL OUTLET.
Same as TIDAL FLATS.
The interval of time between two consecutive, like phases of the TIDE. (See Figure II-5-16.)
A pool of water remaining on a beach or reef after recession of the TIDE.
(1) The total amount of water that flows into a harbor or out again with movement of the tide, excluding any fresh water flow. (2) The volume of water present between MEAN LOW and MEAN HIGH TIDE.
The difference in height between consecutive high and low (or HIGHER HIGH and LOWER LOW) waters. (See Figure II-5-16.)
The height of tide as referred to the datum of a chart. (See Figure II-5-16.)
That part of a river where the water level is influenced by the tide.
Shoals that accumulate near inlets due to the transport of sediments by tidal currents associated with the INLET.
An interval at high or low water when there is no observable change in the height of the tide. The water level is stationary at high and low water for only an instant, but the change in level near these times is so slow that it is not usually perceptible.
(1) The wave motion of the tides. (2) In popular usage, any unusually high and destructive water level along a shore, usually referring to STORM SURGE or TSUNAMI, which are not tidal phenomena at all.
TIDALLY DRIVEN CIRCULATION
The movement of fresh water and seawater that are mixed by the sloshing back and forth of the ESTUARY in response to ocean tides.
The periodic rising and falling of the water that results from gravitational attraction of the Moon and Sun and other astronomical bodies acting upon the rotating Earth. Although the accompanying horizontal movement of the water resulting from the same cause is also sometimes called the tide, it is preferable to designate the latter as TIDAL CURRENT, reserving the name TIDE for the vertical movement.
TIDE, DAILY RETARDATION OF
The amount of time by which corresponding tides grow later day by day (about 50 minutes). Also LAGGING.
A tide with one high water and one low water in a day. (See Figure II-5-16)
See EBB TIDE.
See FLOOD TIDE.
See MIXED TIDE.
See NEAP TIDE.
See SEMIDIURNAL TIDE.
See SLACK TIDE.
See SPRING TIDE.
A tide gage consisting of a vertical graduated staff from which the height of the tide can be read directly. It is called a fixed staff when it is secured in place so that it cannot be easily removed. A portable staff is designed for removal from the water when not in use.
A place at which tide observations are being taken. It is called a primary tide station when continuous observations are to be taken over a number of years to obtain basic tidal data for the locality. A secondary tide station is one operated over a short period of time to obtain data for a specific purpose.
See STORM SURGE.
Tables which give daily predictions of the times and heights of the tide. These predictions are usually supplemented by tidal differences and constants by means of which additional predictions can be obtained for numerous other places.
See WIND TIDE.
The zone between the MEAN HIGH WATER line and the MEAN LOW WATER line, commonly referred to as the BEACH. Waters above the tidelands are inland, being landward of the COAST LINE.
Lowest part of sea- and portside BREAKWATER slope, generally forming the transition to the seabed..
A bar or spit that connects an island to the mainland or to another island. See CUSPATE SPIT. (See Figure IV-1-6.). Also applied to sand accumulation between land and a DETACHED BREAKWATER.
A long narrow strip of land, projecting into a body of water.
A map on which elevations are shown by means of contour lines.
The configuration of a surface, including its relief and the positions of its streams, roads, building, etc.
A wall or jetty to direct current flow.
The invasion of a large area of land by the sea in a relatively short space of time (geologically speaking). Although the observable result of a marine transgression may suggest an almost ‘instantaneous’ process, it is probable that the time taken is in reality is thousands or millions of years. The plane of marine transgression is a plane of UNCONFORMITY.
TRANSITIONAL ZONE (TRANSITIONAL WATER)
In regard to progressive gravity waves, water whose depth is less than ½ but more than 1/25 the wavelength. Often called shallow water.
See WAVE OF TRANSLATION.
See HYPOTHETICAL HURRICANE.
A bar which extends approximately right angles to shorelines.
Waves that propagate along a sailing line of a vessel. (See Figure II-7-40)
A long narrow submarine depression with relatively steep sides.
A theoretical, progressive oscillatory wave first proposed by Gerstner in 1802 to describe the surface profile and particle orbits of finite amplitude, nonsinusoidal waves. The wave form is that of a prolate cycloid or trochoid, and the fluid particle motion is rotational as opposed to the usual irrotational particle motion for waves generated by normal forces. Compare IRROTATIONAL WAVE
A tropical cyclone with maximum winds less than 34 m/sec (75 mile per hour). Compare with HURRICANE or
TYPHOON (winds greater than 34 m/sec).
A long and broad submarine DEPRESSION with gently sloping sides.
TROUGH OF WAVE
The lowest part of a waveform between successive crests. Also, that part of a wave below still-water level.
A long-period water wave caused by an underwater disturbance such as a volcanic eruption or earthquake. Also
SEISMIC SEA WAVE. Commonly miscalled "tidal wave."
(1) A condition of a liquid due to fine visible material in suspension, which may not be of sufficient size to be seen as individual particles by the naked eye but which prevents the passage of light through the liquid. (2) A measure of fine suspended matter in liquids.
A flowing mass of sediment-laden water that is heavier than clear water and therefore flows downslope along the
bottom of the sea or a lake.
Any flow which is not LAMINAR, i.e., the stream lines of the fluid, instead of remaining parallel, become confused and intermingled.
See HURRICANE. The term typhoon is applied to tropical cyclones in the western Pacific Ocean.
A surface that represents a break in the geologic record, with the rock unit immediately above it being considerably younger than the rock beneath. There are three major aspects to consider: (1) Time. An unconformity develops during a period of time in which no sediment is deposited. This concept equates deposition and time, and an unconformity represents unrecorded time. (2) Deposition. Any interruption of deposition, whether large or small in extent, is an unconformity. This aspect of unconformity pre-supposes a standard ‘scale’ of deposition which is complete. Major breaks in sedimentation can usually be demonstrated easily, but minor breaks may go unrecorded until highly detailed investigations are made. (3) Structure. Structurally, unconformity may be regarded as planar structures separating older rocks below from younger rocks above, representing the ‘break’ as defined in (1) and (2) above. A plane of unconformity may be a surface of weathering, Erosion or denudation, or a surface of non-deposition, or possibly some combination of these factors. It may be parallel to the upper strata, make an angle with the upper strata, or be irregular. Subsequent Earth movements may have folded or faulted it.
In referring to sediment grains, loose, separate, or unattached to one another.
Erosion of material at the foot of a cliff or bank, e.g., a sea cliff, or river bank on the outside of a meander. Ultimately, the overhang collapses, and the process is repeated.
(1) A current below water surface flowing seaward; the receding water below the surface from waves breaking on a shelving beach. (2) Actually undertow is largely mythical. As the BACKWASH of each wave flows down the BEACH, a current is formed which flows seaward. However, it is a periodic phenomenon. The most common phenomena expressed as “undertow” are actually RIP CURRENTS.
The slope of the sea bottom. See SLOPE.
UNDISTURBED WATER LEVEL
Same as STILL WATER LEVEL.
A continuously propagated motion to and fro, in any fluid or elastic medium, with no permanent translation of the particles themselves.
In United States usage, the coastal direction generally trending toward the north.
The direction opposite that of the predominant movement of littoral materials.
Dry land area above and landward of the ORDINARY HIGH WATER MARK (OHWM). Often used as a general term to mean high land far from the COAST and in the interior of the country.
The upward water pressure on the base of a structure or pavement.
The rush of water up the FORESHORE following the breaking of a wave, also called SWASH or RUNUP.
Along coasts with obliquely approaching waves there is a longshore (wave-driven) current. For this current one can define an upstream and a DOWNSTREAM direction. For example, on a beach with an orientation west-east with the sea to the north, the waves come from NW. Then the current flows from West to East. Here, upstream is West of the observer, and East is DOWNSTREAM of the observer.
The process by which water rises from a deeper to a shallower depth, usually as a result of offshore surface water flow. It is most prominent where persistent wind blows parallel to a coastline so that the resultant Ekman transport moves surface water away from the coast.
An elongated depression, usually with an outlet, between BLUFFS or between ranges of hills or mountains.
A prolongation of a land valley into or across a continental or insular shelf, which generally gives evidence of having been formed by stream erosion.
VELOCITY OF WAVES
The speed at which an individual wave advances. See WAVE CELERITY.
The velocity gradient within the BOTTOM BOUNDARY LAYER, displayed as a graph of height above the bed against the velocity of the flow.
VISCOSITY (or internal friction)
That molecular property of a fluid that enables it to support tangential stresses for a finite time and thus to resist deformation. Resistance to flow.
For a sediment sample, defined as the ratio of the volume of the voids to the volume of the solids, Q = Vv/Vs. Typical values of Q for natural sands range from 0.5 to 0.8, for cohesive soils from 0.7 to 1.1.
Part of the suspended load with particle sizes smaller than found in the bed; it is in near-permanent suspension and transported without deposition; the amount of wash load transported through a reach does not depend on the transport capacity of the flow; the load is expressed in mass or volume per unit of time.
Sediment deposited inland of a beach by overwash processes.
Distance between the seabed and the still water level.
Elevation of still water level relative to some datum.
A juncture of land and sea. This line migrates, changing with the tide or other fluctuation in the water level. Where waves are present on the beach, this line is also known as the limit of backrush (approximately, the intersection of the land with the still-water level.)
A ridge, deformation, or undulation of the surface of a liquid.
The ratio of wave speed to wind speed.
The speed of wave propagation.
The seasonal and annual distribution of wave height, period and direction.
WAVE CLIMATE ATLAS
Series of maps showing the variability of wave conditions over a long coastline.
See CREST OF WAVE.
WAVE CREST LENGTH
See CREST LENGTH, WAVE.
See CYCLOIDAL WAVE.
See DECAY OF WAVES.
The direction from which a wave approaches.
WAVE DIRECTIONAL SPECTRUM
Distribution of wave energy as a function of wave frequency and direction.
The theoretical determination of future wave characteristics, usually from observed or predicted meteorological phenomena.
The inverse of wave period.
WAVE FREQUENCY SPECTRUM
Distribution of wave energy as a function of frequency.
See GRAVITY WAVE.
A series of waves in which the wave direction, wavelength, and wave height vary only slightly. See also GROUP VELOCITY.
The vertical distance between a crest and the preceding trough. See also SIGNIFICANT WAVE HEIGHT.
WAVE HEIGHT COEFFICIENT
The ratio of the wave height at a selected point to the deepwater wave height. The REFRACTION COEFFICIENT multiplied by the shoaling factor.
See HINDCASTING, WAVE.
See INFRAGRAVITY WAVE.
See IRROTATIONAL WAVE.
See MONOCHROMATIC WAVES.
WAVE OF TRANSLATION
A wave in which the water particles are permanently displaced to a significant degree in the direction of wave travel. Distinguished from an OSCILLATORY WAVE.
See OSCILLATORY WAVE.
WAVE PEAK FREQUENCY
The inverse of wave peak period.
The time for a wave crest to traverse a distance equal to one wavelength. The time for two successive wave crests to pass a fixed point. See also SIGNIFICANT WAVE PERIOD.
See PROGRESSIVE WAVE.
The transmission of waves through water.
That part of an incident wave that is returned seaward when a wave impinges on a steep beach, barrier, or other reflecting surface.
See REFRACTION (of water waves).
Diagram showing the long-term distribution of wave height and direction.
Drop in water level outside of the breaker zone to conserve momentum as wave particle velocities and pressures change prior to wave breaking.
See SETUP, WAVE.
An oscillatory wave having the form of a sinusoid.
See SOLITARY WAVE.
In ocean wave studies, a graph, table, or mathematical equation showing the distribution of wave energy as a function of wave frequency. The spectrum may be based on observations or theoretical considerations. Several forms of graphical display are widely used.
See STANDING WAVE.
The ratio or wave height to wavelength also known as sea steepness.
A series of waves from the same direction.
Change in wave energy due to the action of physical processes.
See TROCHOIDAL WAVE.
The lowest part of a wave form between successive crests. Also that part of a wave below still-water level.
The speed at which an individual wave advances.
See WIND WAVES.
The horizontal distance between similar points on two successive waves measured perpendicular to the crest.
See INTERNAL WAVES.
A model probability distribution, commonly used in wave analysis.
A low dam or wall across a stream to raise the upstream water level. Termed fixed crest weir when uncontrolled.
A jetty with a low section or weir over which littoral drift moves into a predredged deposition basin which is then dredged periodically.
Lands whose saturation with water is the dominant factor determining the nature of soil development and the types of plant and animal communities that live in the soil and on its surface (e.g. Mangrove forests).
Clastic sediment or rock that consists of particles all having approximately the same size. Example: sand dunes.
A structure built on the shore of a harbor, river, or canal, so that vessels may lie alongside to receive and discharge cargo and passengers.
On the crest of a wave, the white froth caused by wind.
Bundles of twigs or sticks, often willow, used in building earthworks or levees (traditional practice in Holland and China.). Alternate term: fascine
See FOLLOWING WIND.
See KATABATIC WIND
A wind blowing seaward from the land in a coastal area.
A wind blowing landward from the sea in a coastal area.
See OPPOSING WIND.
Diagram showing the long-term distribution of wind speed and direction.
Wave conditions directly attributable to recent winds, as opposed to swell.
Drop in water level below the still water level on the windward ends of enclosed bodies of water and semi- enclosed bays.
On reservoirs and smaller bodies of water (1) the vertical rise in the still-water level on the leeward side of a body
of water caused by wind stresses on the surface of the water; (2) the difference in still-water levels on the windward and the
leeward sides of a body of water caused by wind stresses on the surface of the water. STORM SURGE (usually reserved for
use on the ocean and large bodies of water).
The way in which wind transfers energy to the sea surface.
See WIND SETUP, STORM SURGE.
(1) Waves being formed and built up by the wind. (2) Loosely, any wave generated by wind.
The direction from which the wind is blowing.
Bowles, J. E. 1979. Physical and Geotechnical Properties of Soils. McGraw Hill, New York, 465 p. Hicks 1989
Hicks S. 1989. Tide and Current Glossary, National Ocean Service, National Oceanic and Atmospheric Administration, U.S. Department of Commerce. Jackson and Bates (ed.) 1984
Jackson, J. A., and Bates, R. L. (editors). 1984. Dictionary of Geological Terms, Third Edition. Anchor Press/Doubleday, Garden City, NY NOAA Coastal Services Center 2001
NOAA Coastal Services Center. 2001. Shoreline Mapping Web Site, Shoreline Terms, United States Department of Commerce, National Oceanic and Atmospheric Administration, National Ocean Service, Charleston, SC (http://www.csc.noaa.gov/shoreline/term.html , 30 August 2001)
Reed, M. 2000. Shore and Sea Boundaries, Volume 3, The Development of International Maritime Boundary Principles through United States Practice. U.S. Department of Commerce, National Oceanic and Atmospheric Administration. Washington, D.C: U.S. Government Printing Office, 432 p. (Also available online at http://chartmaker.ncd.noaa.gov/hsd/shallow.htm) Shore Protection Manual 1984
Shore Protection Manual. 1984. 4th ed., 2 Vol., U.S. Army Engineer Waterways Experiment Station, U.S. Government Printing Office, Washington, D.C., 1,088 p.
Verhagen, H. J. 1998. Glossary of Coastal Engineering Terms, Department of Hydraulic Engineering, International Institute for Infrastructural, Hydraulic, and Environmental Engineering, Delft, The Netherlands (http://www.ihe.nl/he/dicea/int01/glossary.htm , 30 August 2001) Voight 1998
Voigt, B. 1998. Glossary of Coastal Terminology, Pub. No. 98-105, Washington State Department of Ecology, Olympia, WA ( http://www.csc.noaa.gov/text/glossary.html , 30 Aug. 2001) Webster’s Third New International Dictionary of the English Language Unabridged 1981
Webster’s Third New International Dictionary of the English Language Unabridged. 1981. G. & C. Merriam Company, Springfield, MA. Wiegel 1953
Wiegel, R. L. 1953. Waves, Tide, Currents, and Beaches: Glossary of Terms and List of Standard Symbols, Council on Wave Research, The Engineering Foundation, Berkeley, CA.
Dr. Andrew Morang, Coastal and Hydraulics Laboratory, U.S. Army Engineer Research and Development Center, Vicksburg, MS.
Mr. Andre Szuwalski, Coastal and Hydraulics Laboratory, U.S. Army Engineer Research and Development Center, Vicksburg, MS (retired). Reviewers:
Mr. John H. Lockhart, Jr., Headquarters, U.S. Army Corps of Engineers, Washington, D.C. (retired).
Mr. Orville Magoon, Coastal Zone Foundation, Middletown, CA.
Dr. Joan Oltman-Shay, Northwest Research Associates, Inc., Bellevue, WA.
Ms. Joan Pope, Coastal and Hydraulics Laboratory, U.S. Army Engineer Research and Development Center,
Comments or additions: Please contact Dr. Andrew Morang at tel: 601 634 2064 or email email@example.com with comments on errors or omissions in this glossary.
Last editorial update: 24 April 2003.