首页|Aerosol Direct Radiative Forcing over Shandong Peninsula in East Asia from 2004 to 2011

Aerosol Direct Radiative Forcing over Shandong Peninsula in East Asia from 2004 to 2011

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Recent vigorous industrialization and urbanization in Shandong Peninsula,China,have resulted in the emission of heavy anthropogenic aerosols over the region.The annual means of aerosol optical depth (AOD),Angstrom exponent (α),single-scattering albedo (SSA),aerosol direct radiative forcing (ARF),surface radiative forc ing (SRF),and top-of-the atmospheric radiative forcing(TOA) recorded during 2004-2011 were respectively 0.67±0.19,1.25±0.24,0.93±0.03,47±9 W m-2,-61±9 W m-2,and-14±8 W m-2.The aerosol optical properties and ARF characteristics showed remarkable seasonal variations due to cycle changes in the aerosol components and dominance type.The atmosphere-surface system was cooled by ARF in all years of the study due to anthropogenic sulfate and nitrate emission and sea salt aerosols.The magnitude of TOA cooling was larger in summer (-15±17 W m-2) and autumn (-12±7 W m-2) than that in spring (-8±4 W m 2) and winter (-9±10 W m-2).

aerosol optical depth(A)ngstr(o)m exponentsingle scattering albedoaerosol direct radiative forcingShandong Peninsula

XIN Jin-Yuan、ZHANG Qing、GONG Chong-Shui、WANG Yue-Si、DU Wu-Peng、ZHAO Yong-Fang

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State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry(LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China

China Communication Information Center, Beijing 100088, China

Beijing Municipal Climate Center, Beijing Meteorological Service, Beijing 100089, China

Jiaozhou Bay Marine Ecosystem Research Station, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China

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National Natural Science Foundation of ChinaStrategic Priority Research Program of the Chinese Academy of Sciences

41222033,41375036,and 41105103XDA05100102 and XDB05020103

2014

大气和海洋科学快报(英文版)
中国科学院大气物理研究所

大气和海洋科学快报(英文版)

CSCD
影响因子:0.465
ISSN:1674-2834
年,卷(期):2014.7(1)
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