Science. 1980 Aug 1;209(4456):595-7. doi: 10.1126/science.209.4456.595.
Satellite and research vessel observations of sea surface temperature during the southwest monsoon of 1979 show the development of large wedge-shaped areas of cold water along the Somali coast at both 5 degrees and 10 degrees N during June and July. The cold water associated with the large northern and southern Somali eddy systems could be traced several hundred kilometers offshore. By late August the cold wedge at 5 degrees N translated northeastward as far as 10 degrees N at speeds of 15 to 30 centimeters per second, indicating a coalescence of the systems.
卫星和研究船对 1979 年西南季风期间的海面温度的观测显示,在 6 月和 7 月,北纬 5 度和 10 度的索马里沿岸出现了大型楔形冷水区域。与北、南索马里反气旋涡系统相关的冷水可以在离岸几百公里的地方被追踪到。到 8 月底,5 度 N 的冷楔以 15 到 30 厘米/秒的速度向东北方向移动,最远到达 10 度 N,表明两个系统正在合并。