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INTERACTION BETWEEN SEA SURFACE TEMPERATURE AND ATMOSPHERIC CIRCULATION IN WINTER HALF YEAR
引用本文:王绍武,赵宗慈,陈振华,魏松林,于平书. INTERACTION BETWEEN SEA SURFACE TEMPERATURE AND ATMOSPHERIC CIRCULATION IN WINTER HALF YEAR[J]. 海洋学报(英文版), 1982, 1(2): 189-194
作者姓名:王绍武  赵宗慈  陈振华  魏松林  于平书
作者单位:Department of Geophysics,Peking University,Department of Geophysics,Peking University,Department of Geophysics,Peking University,Department of Geophysics,Peking University,Department of Geophysics,Peking University
摘    要:As oceans cover about 71% of the Earth's surface and have bigger thermal capacitythan the air, they act as a storage and regulator of solar radiation, and therefore, playan important part in the formation of long-range weather process. Many meteorologistshave been studying the interaction between the sea surface temperature (SST) and theatmospheric circulation. Some of them emphasize the active role of the oceans andconsider that the variations of SST control the atmospheric circulation anomalies, butothers often express different viewpoints. What relation really exists between the oceanand the atmosphere? To answer this question, one must pay more attention to the spatialand temporal variations in the relationship between circulation and SST. The purposeof the present paper is to get a better understanding of their variations.

收稿时间:1981-08-28

INTERACTION BETWEEN SEA SURFACE TEMPERATURE AND ATMOSPHERIC CIRCULATION IN WINTER HALF YEAR
WANG SHAOWU,ZHAO ZONGCI,CHEN ZHENHUA,WEI SONGLIN and YU PINGSHU. INTERACTION BETWEEN SEA SURFACE TEMPERATURE AND ATMOSPHERIC CIRCULATION IN WINTER HALF YEAR[J]. Acta Oceanologica Sinica, 1982, 1(2): 189-194
Authors:WANG SHAOWU  ZHAO ZONGCI  CHEN ZHENHUA  WEI SONGLIN  YU PINGSHU
Affiliation:Department of Geophysics, Peking University
Abstract:As oceans cover about 71% of the Earth's surface and have bigger thermal capacity than the air, they act as a storage and regulator of solar radiation, and therefore, play an important part in the formation of long-range weather process.Many meteorologists have been studying the interaction between the sea surface temperature (SST) and the atmospheric circulation[1-5].Some of them emphasize the active role of the oceans and consider that the variations of SST control the atmospheric circulation anomalies, but others often express different viewpoints.What relation really exists between the ocean and the atmosphere? To answer this question, one must pay more attention to the spatialand temporal variations in the relationship between circulation and SST.The purpose of the present paper is to get a better understanding of their variations.
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