论世界海洋的深海环流——四

Bert Bolin , Henry Stommel
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引用次数: 150

摘要

利用箱形模型,以及观测到的温度、盐度和放射性碳分布,对构成太平洋和印度洋共有水以及南极中间水的水的来源和流速进行了估计。介绍了将计算推广到南极底水的困难。重点放在计算可靠性和“病态”方程的出现问题上。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
On the abyssal circulation of the world ocean—IV

Using box models, and the observed distribution of temperature, salinity and radiocarbon estimates are made of the origins and rate of flow of waters that make up the Common Water in the Pacific and Indian Oceans, and Antarctic Intermediate Water. Difficulties in extending the computation to Antarctic Bottom Water are described. Emphasis is placed upon questions of computational reliability and the occurrence of ‘ill-conditioned’ equations.

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