| Direct Climatic Effect of Dust Aerosol in the NCAR Community Atmosphere Model Version 3 （CAM3） |
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| 引用本文： | YUE Xu,WANG Huijun,LIAO Hong,FAN Ke. Direct Climatic Effect of Dust Aerosol in the NCAR Community Atmosphere Model Version 3 （CAM3）[J]. 大气科学进展, 2010, 27(2): 230-242. DOI: 10.1007/s00376-009-8170-z |
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| 作者姓名： | YUE Xu WANG Huijun LIAO Hong FAN Ke |
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| 作者单位： | Climate;Change;Research;Center;Chinese;Academy;Sciences;Nansen-Zhu;International;（NZC）;Institute;Atmospheric;Physics;Graduate;University;State;Laboratory;Boundary;Layer;Chemistry; |
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| 基金项目： | supported by the Key Project of Chinese Academy of Sciences under Grant KZCX2-YW-Q11-03;;supported by the National Basic Research Program of China (“973” program) under Grant2006CB403705;;the Key Project of Chinese Academy of Sciences under Grants KZCX2-YW-Q1-02, KZCX2-YW-205, and KZCX2-YW-219;;the National Natural Science Foundation of China under Grant No. 40631005 |
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| 摘 要： | ![]()
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| 关 键 词： | 沙尘气溶胶 NCAR 气氛 气候效应 版本 模型 社会 粉尘 |
Direct Climatic Effect of Dust Aerosol in the NCAR Community Atmosphere Model Version 3 (CAM3) |
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| YUE Xu,WANG Huijun,LIAO Hong and FAN Ke. Direct Climatic Effect of Dust Aerosol in the NCAR Community Atmosphere Model Version 3 (CAM3)[J]. Advances in Atmospheric Sciences, 2010, 27(2): 230-242. DOI: 10.1007/s00376-009-8170-z |
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| Authors: | YUE Xu WANG Huijun LIAO Hong FAN Ke |
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| Affiliation: | Climate Change Research Center,Chinese Academy of Sciences,Beijing 100029Nansen—Zhu International Research Center(NZC),Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029。Graduate University of the Chinese Academy of Sciences |
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| Abstract: | ![]()
Direct climate responses to dust shortwave and longwave radiative forcing (RF) are studied using the NCAR Community Atmosphere Model Version 3 (CAM3). The simulated RF at the top of the atmosphere (TOA) is-0.45 W m-2 in the solar spectrum and +0.09 W m-2 in the thermal spectrum on a global average. The magnitude of surface RF is larger than the TOA forcing, with global mean shortwave forcing of-1.76 W m-2 and longwave forcing of +0.31 W m-2 . As a result, dust aerosol causes the absorption of 1.1 W m-2 in t... |
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| Keywords: | dust aerosol radiative forcing direct radiative effect general circulation model |
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