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《Chinese Journal of Geophysics》 2005-06
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A preliminary simulation study of direct radiative forcing of mineral dust aerosol over the East Asia region

WU Jian~(1,2),FU Cong-Bin~2,JIANG Wei-Mei~3,LIU Hong-Nian~3,ZHAO Run-Hua~11 Department of Atmospheric Science,Yunnan University,Kunming 650091,China2 Key Laboratory of Regional Climate-Environment Research for Temperate East Asia,Institute of Atmospheric Science,Chinese Academy of Sciences,Beijing 100029,China3 Department of Atmospheric Science,Nanjing University,Nanjing 210093,China  
To study the direct radiative effect of dust aerosol over the East Asia region,a dust emission scheme,a transport model and a radiative scheme of dust aerosol have been added into the Regional Climate Model Version 3(RegCM3).Based on the simulation for the period from March 2001 to February 2002,it has been found that Northwest China and Mongolia are the main dust sources in East Asia,whose emission rates exceed 1μg/(m~2\5s) with maximum value of 90μg/(m~2·s).The maximum column burden of dust aerosol is about 5g/m~2,which emerges over the Taklimakan desert and the Qinling Mountains.The direct radiative forcing at TOA is positive over land and negative or positive over sea,and its regional average values in Spring,Summer,Autumn,and Winter are 1.08,0.88,0.37,0.40W/m~2,respectively.The solar radiative forcing is also positive over land and negative or positive over sea, but the infrared radiative forcing is positive in the modeling region.The radiative forcing values at the surface for four seasons are-5.64,-2.25,-1.37,(-1.87W/m~2,) respectively.Radiative forcing is affected sensitively by the change of single scattering albedo of dust aerosol.
【Fund】: 国家自然科学基金(40205016);; 中国博士后科学基金(2004036295);; 云南省自然科学基金(2003D0011)资助
【CateGory Index】: X513;
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