Simulation of Direct Radiative Forcing of Aerosols and Their Effects on East Asian Climate Using an Interactive AGCM-aerosol Coupled System
An interactive system coupling the Beijing Climate Center atmospheric general circulation model (BCC_AGCM2.0.1) and the Canadian Aerosol Module (CAM) was developed to investigate the global distributions of optical properties and direct radiative forcing (DRF) of typical aerosols and their impacts on East Asian climate. Under all-sky conditions, the simulated global annual means of sulfate, BC, and OC DRF at the TOA were -0.19 W m-2, +0.1 W m-2, and -0.15 W m-2, respectively. The sulfate, BC, and OC aerosols led to decreases of 0.58 oC and 0.14 mm day-1 in the JJA means of surface temperature and precipitation rate in East Asia. The differences of land-sea surface temperature and surface pressure were reduced in East Asian monsoon region due to these aerosols, thus leading to the weakening of East Asian summer monsoon. Atmospheric dynamic and thermodynamic were affected due to the three types of aerosol, and the southward motion between 15oN and 30o N in lower troposphere was increased, which slowed down the northward transport of moist air carried by the East Asian summer monsoon, and moreover decreased the summer monsoon precipitation in south and east China.
AGCM Aerosol Radiative forcing Climate effects East Asian monsoon
Hua Zhang Zhili Wang
National Climate Center,China Meteorological Administration,No. 46 Zhongguancun Nandajie Haidian Dis Chinese Academy of Meteorological Sciences,No. 46 Zhongguancun Nandajie Haidian District,Beijing,Chi
国际会议
西安
英文
251-258
2011-08-17（万方平台首次上网日期，不代表论文的发表时间）