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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Cross-shore variation of long-term average longshore current velocity in the nearshore zone
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Cross-shore variation of long-term average longshore current velocity in the nearshore zone

机译:近岸区域长期平均近岸流速的跨岸变化

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The cross-shore variation of long-term average longshore current velocity was investigated on the basis of a 15-year data set of longshore current, wave and wind. The longshore current velocities were measured once a day along a 427-m-long pier. The results show that the direction of the long-term average longshore current velocity away (> 200 m) from the shore was the opposite to that near the shore. The southward current was dominant offshore, whereas the northward current was dominant near the shore. The cross-shore variation of the long-term average longshore current velocity was formed owing to a difference between the wave and wind conditions when the northward and southward currents developed. When the northward current developed, the offshore wave height was relatively small and the frequency of the southward wind velocity was almost equal to that of the northward one. As a result, the northward current developed only near the shore and decayed outside the narrow surf zone. On the other hand, when the southward current developed, the offshore wave height was relatively large and the southward wind velocity was predominant, which resulted in the southward current developing not only in the wide surf zone but also outside the surf zone. The superposition of the two cross-shore variations produced a cross-shore variation of the long-term average longshore current velocity with a northward velocity near the shore and a southward velocity away from the shore. (c) 2007 Elsevier Ltd. All rights reserved.
机译:根据15年的沿岸电流,波浪和风的数据集,研究了长期平均沿岸流速的跨岸变化。每天在427米长的码头上测量一次近岸流速。结果表明,远离海岸的长期平均近岸海流速度(> 200 m)的方向与靠近海岸的方向相反。向南的洋流在海上占主导地位,而向北的洋流在海岸附近占主导地位。长期平均近岸海流速度的跨岸变化是由于南北向水流形成时波浪和风的条件不同而形成的。当向北流形成时,海上波浪高度相对较小,并且向南风速的频率几乎等于向北风速的频率。结果,向北的水流仅在海岸附近发展,并在狭窄的冲浪区外衰减。另一方面,当向南潮流发展时,海上波浪高度相对较大,并且向南风速占优势,这导致向南潮流不仅在宽冲浪区而且在冲浪区之外发展。两种跨岸变化的叠加产生了长期平均近岸流速度的跨岸变化,其中岸边向北速度,岸边向南速度。 (c)2007 Elsevier Ltd.保留所有权利。

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