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An elongated DEPRESSION, usually with an outlet, between BLUFFS or between ranges of hills or mountains.
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(1) The variation of heights and periods between individual waves within a wave train.
(2) The variation in direction of propagation of waves leaving the GENERATING AREA.
(3) The variation in height along the crest, usually called "variation along the wave".
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The velocity gradient within the BOTTOM BOUNDARY LAYER, displayed as a graph of height above the BED against the velocity of the flow.
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