Science. 1969 Mar 28;163(3874):1449-50. doi: 10.1126/science.163.3874.1449.
Measurements of current speed and direction from the sea surface to below 400 meters made on the equator in the eastern Pacific in April 1968 indicate that the Equatorial Undercurrent extends from 300 meters to the sea surface. These measurements, when compared with previous observations, indicate that eastward motion at the surface is a result of surfacing of the undercurrent caused by a release of the surface wind stress.
1968 年 4 月在东太平洋赤道地区进行的从海面到 400 米以下的海流速度和流向测量表明，赤道潜流从 300 米延伸到海面。这些测量结果与以往的观测结果相比表明，表面的向东运动是由于表面风应力释放导致潜流浮出水面而产生的。
