大洋温盐环流的稳定性及变率模拟研究进展

doi:10.11867/j.issn.1001-8166.1998.04.0334

地球科学进展 ›› 1998, Vol. 13 ›› Issue (4): 334 -343. doi: 10.11867/j.issn.1001-8166.1998.04.0334

大洋温盐环流的稳定性及变率模拟研究进展

周天军 ¹，王绍武 ¹，张学洪 ²

1.北京大学地球物理系北京 100871；2.中国科学院大气物理研究所北京 100080

收稿日期:1997-08-14 修回日期:1997-09-29 出版日期:1998-08-01
通讯作者: 周天军
基金资助:
国家自然科学基金项目"20世纪中国与全球气候变率研究"(项目编号:49635190)资助。

PROCEEDING OF MODELLING STUDIES ON THE STABILITY AND VARIABILITY OF THE THERMOHALINE CIRCULATION

Zhou Tianjun ¹，Wang Shaowu ¹，Zhang Xuehong ²

1.Department of Geophysics, Peking University, Beijing 100871；2.Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100080

Received:1997-08-14 Revised:1997-09-29 Online:1998-08-01 Published:1998-08-01

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围绕大洋温盐环流的稳定性和变率，以三维原始方程大洋环流模式（OGCM）和海气耦合模式为重点，兼顾理想概念模式，总结了近年来模拟研究的主要成果。概括了几个主要前沿方向——大洋温盐环流的多平衡态现象、数十年／年代际变率以及百年到千年尺度的变率特性等的研究成果，探讨了其内部机制。

关键词: 温盐环流, 多平衡态, 变率

In this paper, some recent contributions of both primitive equation ocean circulation models(OGCM) and idealized conceptual models to the understanding of the stability and variability properties of the ocean thermohaline circulation are reviewed. The typical results of a hierarchy of models have been represented in brevity. Emphasis has been put on the multiple steady states and variability from decadal/interdecadal timescale to centennial and millennial timescale of the world ocean thermohaline circulation.

Key words: Thermohaline circulation, Mutiple steady states, Variability.

中图分类号:

P733

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