朝一定方向运动的稳定的海水流。

The steady flow of ocean water in a prevailing direction.

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考虑了基础与地基、上部结构及海水流体间的功力相互作用。

The interactions of foundation with base, superstructure and the fluid are considered.

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他认为，可能冰川底下的海水流动是造成此次冰山断裂的主要原因之一。

The flow of sea water below the glaciers is one of the main causes of ice calvings off Greenland.

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