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THE COOLING OF SICHUAN PROVINCE IN RECENT 40 YEARS AND ITS PROBABLE MECHANISMS
作者姓名:Li Xiaowen  Zhou Xiuji  Li Weiliang  Chen Longxun
作者单位:Chinese Academy of Meteorological Sciences Beijing 100081,Chinese Academy of Meteorological Sciences,Beijing 100081,Chinese Academy of Meteorological Sciences,Beijing 100081,Chinese Academy of Meteorological Sciences,Beijing 100081
摘    要:The analysis of temperature variation trends at 160 meteorological stations in China from 1951 to 1992 showed thata relatively large area of China became warm in recent years,but there still existed an obvious cooling center in Sichuanbasin.We also analyzed the variation trends of some meteorological factors which could probably cause this cooling,and the results indicated that the global solar radiation,the insolation duration and the visual range decreased sharply inrecent years,but the cloud amount changed slightly in Sichuan basin.We also found that the decrease of surface solarradiation caused by the increase of the anthropogenic aerosols' backscattering in the lower troposphere was a notablereason for the cooling of Sichuan basin in recent years.We also confirmed this conclusion by using of a one-dimensionalclimate model.

收稿时间:1994/4/20 0:00:00
修稿时间:1994/10/10 0:00:00

THE COOLING OF SICHUAN PROVINCE IN RECENT 40 YEARS AND ITS PROBABLE MECHANISMS
Li Xiaowen,Zhou Xiuji,Li Weiliang,Chen Longxun.THE COOLING OF SICHUAN PROVINCE IN RECENT 40 YEARS AND ITS PROBABLE MECHANISMS[J].Acta Meteorologica Sinica,1995,9(1):57-68.
Authors:Li Xiaowen  Zhou Xiuji  Li Weiliang and Chen Longxun
Institution:Li Xiaowen Zhou Xiuji Li Weiliang Chen Longxun Chinese Academy of Meteorological Sciences,Beijing 100081
Abstract:The analysis of temperature variation trends at 160 meteorological stations in China from 1951 to 1992 showed that a relatively large area of China became warm in recent years,but there still existed an obvious cooling center in Sichuan basin.We also analyzed the variation trends of some meteorological factors which could probably cause this cooling, and the results indicated that the global solar radiation,the insolation duration and the visual range decreased sharply in recent years,but the cloud amount changed slightly in Sichuan basin.We also found that the decrease of surface solar radiation caused by the increase of the anthropogenic aerosols' backscattering in the lower troposphere was a notable reason for the cooling of Sichuan basin in recent years.We also confirmed this conclusion by using of a one-dimensional climate model.
Keywords:Sichuan basin  cooling  mechanism  aerosol
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