ATMOSPHERIC FEEDBACK IN A COUPLED OCEAN-ATMOSPHERE MODEL

被引：2

作者：

WELLS, NC ^{[1
]}

PURI, K ^{[1
]}

机构：

[1] AUSTRALIAN NUMERICAL METEOROL RES CTR, MELBOURNE 3000, VICTORIA, AUSTRALIA

来源：

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS | 1979年 / 84卷 / NC8期

关键词：

D O I：

10.1029/JC084iC08p04971

中图分类号：

P7 [海洋学];

学科分类号：

0707 ;

摘要：

The model is integrated for a period of 72 days for fixed January radiation conditions. The main feature of the model is a warming trend which occurs throughout the period in both the ocean and the atmosphere. This is shown to be due to the excess solar radiation at all latitudes, which causes an increase in sea surface temperature (SST), with the maximum increase of 3oK occurring between 30oS and 40oS. As a consequence, the evaporation is increased in middle latitudes, and the resultant increased water vapor is transported to the equatorial region and higher latitudes, where condensation causes a warming of the troposphere.- from Authors

引用

页码：4971 / 4984

页数：14

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