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Limits Of The Existence Of The Kuroshio And Gulf Stream Currents Owing To Climate Trends

机译:气候趋势导致黑潮和墨西哥湾流的存在极限

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摘要

Based on the variational property of the energy scattering minimum, this paper presents a model of a zonal jet current applied to the Kuroshio Extension and Gulf Stream after their separation from the western boundary and their turning to the east. The model suggests the following features: (1) the condition of jet existence is the asymmetric current shape with a sharp northern boundary; (2) the dynamic current axis is located south of the convergence axis (this is one of the mechanisms of the formation of two-(multi)front structures in the ocean represented by the Subarctic Front and Kuroshio Extension); and (3) there is a critical parameter range beyond which the current is not the jet current anymore. The modern climate wanning tendency is approaching a critical state, when a change in the circulation structure is expected.
机译:基于能量散射最小值的变化特性,本文提出了黑潮扩展和墨西哥湾流从西部边界分离并向东转向后施加的区域性射流的模型。该模型具有以下特征:(1)喷流存在的条件是具有不规则的北边界的不对称电流形状; (2)动态电流轴位于会聚轴以南(这是由亚弧前缘和黑潮扩展代表的海洋中两(多)前锋结构形成的机制之一); (3)存在一个关键参数范围,超出该范围电流不再是喷射电流。当预期循环结构发生变化时,现代气候减弱趋势已接近临界状态。

著录项

  • 来源
    《Doklady Earth Sciences》 |2008年第3期|p.527-530|共4页
  • 作者

    T. R. Kilmatov;

  • 作者单位

    Pacific Institute of Oceanology, Far East Division, Russian Academy of Sciences, ul. Baltiiskaya 43, Vladivostok, 690041 Russia;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 天文学、地球科学;
  • 关键词

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