A diagnostic model of the sea surface winds and a computational model of the ocean surface currents are developed in this paper.
设计了一个海面风场的诊断模式和一个海洋表层流的数值计算模式。
The ocean surface currents driven by the sea surface winds and the sea surface pressure fields are also close to the observations.
用海面风场和海面气压场启动的海洋表面流，与实况也较一致。
The sea surface winds and the ocean surface currents can be obtained by iteration method as long as the sea surface level pressure fields are input.
只要输入海面气压场并利用迭代方法，即可求得海洋表面的风场和海流场。
Besides being steady and strong, downslope winds can also be cold, and the frigid wind over the ocean surface has helped form fresh sea ice in areas where older ice was blown out to sea.
下行风除了强烈和稳定，还具有低温的特点，这股寒流风吹过海面之后，在那些已形成海冰被吹出海域的地方，新的海冰就形成了。
Besides being steady and strong, downslope winds can also be cold, and the frigid wind over the ocean surface has helped form fresh sea ice in areas where older ice was blown out to sea.
下行风除了强烈和稳定，还具有低温的特点，这股寒流风吹过海面之后，在那些已形成海冰被吹出海域的地方，新的海冰就形成了。
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