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墨西哥湾流冷核环:它们的物理、化学和生物学。

Gulf stream cold-core rings: their physics, chemistry, and biology.

出版信息

Science. 1981 Jun 5;212(4499):1091-100. doi: 10.1126/science.212.4499.1091.

Abstract

Cyclonic Gulf Stream rings are energetic eddies in the warm Sargasso Sea consisting of a ring of Gulf Stream water surrounding a core of cold Slope Water. Initially a ring core has the characteristics of the Slope Water; it is rich in plants, animals, and nutrients. As a ring decays the Slope Water properties of its core are gradually replaced by those of the Sargasso Sea, where standing crops of plants, animals, and nutrients generally are low. Although the decay rate suggests a rather long lifetime (2 to 4 years), the usual death of a ring comes when it rejoins the Gulf Stream after 6 to 12 months.

摘要

气旋式墨西哥湾流环是马尾藻海温暖水域中的强力漩涡,由一个墨西哥湾流的水环围绕着一个冷的陆坡水核心组成。最初,一个环核心具有陆坡水的特征;它富含植物、动物和营养物质。随着环的衰减,其核心的陆坡水特性逐渐被马尾藻海的特性所取代,那里的植物、动物和营养物质的现存量通常较低。尽管衰减率表明其寿命相当长(2 到 4 年),但一个环通常在 6 到 12 个月后重新加入墨西哥湾流时就会死亡。

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