①在近岸区域自海面向下至1—3米水层的流动；在深海区域，自海面往下至10米水层内的流动。②最大流速所在的流轴位于海面或接近海面的任何海流。③发生于海洋浅层的海。
First, the least square multiplication based basic surface current arithmetic is introduced.
论文先给出基于最小二乘法的表层流基础算法。
参考来源 - X波段雷达海面流场信息提取技术研究First, the least square multiplication based basic surface current arithmetic is introduced.
论文先给出基于最小二乘法的表层流基础算法。
参考来源 - X波段雷达海面流场信息提取技术研究·2,447,543篇论文数据，部分数据来源于NoteExpress
在九州西南海域，黑潮表层流并无分支北上进入对马暖流区。
There was no surface branch of the Kuroshio flowing northward and entering the area of the Tsushima Warm Current, southwest of Kyushu.
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。
A diagnostic model of the sea surface winds and a computational model of the ocean surface currents are developed in this paper.
他们通过2009年的分析数据，发现当表层流动加快，内部的流动却会慢慢停止下来。
Analysing data from 2009, they found that while the surface flows had sped up, the internal ones had slowed to a crawl.
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