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北大西洋亚热带环流:通过锚定监听站追踪的SOFAR浮标

North Atlantic Subtropical Gyre: SOFAR Floats Tracked by Moored Listening Stations.

作者信息

Richardson P L, Price J F, Owens W B, Schmitz W J, Rossby H T, Bradley A M, Valdes J R, Webb D C

出版信息

Science. 1981 Jul 24;213(4506):435-7. doi: 10.1126/science.213.4506.435.

Abstract

In 1980, SOFAR (sound fixing and ranging) floats were tracked acoustically in the western North Atlantic entirely by means of moored autonomous listening stations. During a 5-month period 17 float trajectories were obtained in the eastern (45 degrees to 65 degrees W) Gulf Stream and subtropical gyre interior at depths of 700 and 2000 meters. These mid-depth trajectories suggest a time-varying Gulf Stream with instances of both a narrow, swift, westward recirculation south of the stream and a northeastward penetration into the Newfoundland Basin. A hundredfold increase of eddy kinetic energy was observed at 2000 meters from the gyre interior (south of 30 degrees N) to the Gulf Stream.

摘要

1980年,在北大西洋西部,远距离定位声纳浮标完全通过系泊式自主监听站进行声学跟踪。在为期5个月的时间里,在东(西经45度至65度)墨西哥湾流和亚热带环流内部700米和2000米深处获取了17个浮标轨迹。这些中深度轨迹表明,墨西哥湾流随时间变化,既有在洋流以南狭窄、快速的向西再循环情况,也有向东北方向渗透到纽芬兰盆地的情况。在从环流内部(北纬30度以南)到墨西哥湾流的2000米深处,观测到涡动动能增加了100倍。

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