DEFORMATION OF ROTATIONAL TIDAL CURRENTS IN SHALLOW COASTAL WATER

Harold Gohren

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DEFORMATION OF ROTATIONAL TIDAL CURRENTS IN SHALLOW COASTAL WATER

机译：浅水沿岸旋转潮汐电流的变形

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Along gently sloping coasts of seas having rotary tidal currents, the symmetry of the rotary current is interrupted where the water is shallow As a result, residual counter currents are formed The dynamics of such a current system are described based on current measurements in the Elbe Estuary (southeastern North Sea) The residual currents of this area result in the movement of bottom sediment and are most likely responsible for a series of similar appearing morphologic features.

机译：沿着具有旋转潮流的海洋的缓缓倾斜的海岸，在水很浅的地方中断了旋转电流的对称性。结果，形成了剩余的逆流。基于易北河河口中的电流测量来描述这种电流系统的动力学特性（东南北海）该区域的剩余水流导致底部沉积物的运动，并且很可能是造成一系列相似的形态特征的原因。

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《Proceedings of the International Conference on Coastal Engineering》 |1970年第12期|共页
作者
Harold Gohren;
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机译：浅螺旋壳的小旋转对称变形。

DEFORMATION OF ROTATIONAL TIDAL CURRENTS IN SHALLOW COASTAL WATER

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