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Comments on ``Direct Radiative Forcing of Anthropogenic Aerosols over Oceans from Satellite Observation"


doi: 10.1007/s00376-012-1218-5

  • Previous observational studies have estimated anthropogenic aerosol direct radiative forcing over oceans without due consideration of cloudy-sky aerosols. However, when interaction between clouds and aerosols located below or above the cloud level is taken into account, the aerosol direct radiative forcing is larger by as much as 5 W m-2 in most mid-latitude regions in the Northern Hemisphere.
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    [3] Min ZHAO, Tie DAI, Hao WANG, Qing BAO, Yimin LIU, Hua ZHANG, Guangyu SHI, 2022: Simulating Aerosol Optical Depth and Direct Radiative Effects over the Tibetan Plateau with a High-Resolution CAS FGOALS-f3 Model, ADVANCES IN ATMOSPHERIC SCIENCES, 39, 2137-2155.  doi: 10.1007/s00376-022-1424-8
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    [13] CHEN Lin, SHI Guangyu, QIN Shiguang, YANG Su, ZHANG Peng, 2011: Direct Radiative Forcing of Anthropogenic Aerosols over Oceans from Satellite Observations, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 973-984.  doi: 10.1007/s00376-010-9210-4
    [14] LI Shu, WANG Tijian, ZHUANG Bingliang, HAN Yong, 2009: Indirect Radiative Forcing and Climatic Effect of the Anthropogenic Nitrate Aerosol on Regional Climate of China, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 543-552.  doi: 10.1007/s00376-009-0543-9
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Manuscript History

Manuscript received: 10 January 2013
Manuscript revised: 10 January 2013
通讯作者: 陈斌, bchen63@163.com
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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Comments on ``Direct Radiative Forcing of Anthropogenic Aerosols over Oceans from Satellite Observation"

  • 1. School of Earth and Environmental Sciences, Seoul National University, Seoul, Korea;School of Earth and Environmental Sciences, Seoul National University, Seoul, Korea;Department of Environmental Science and Engineering, Ewha Womans University, Seoul, Korea

Abstract: Previous observational studies have estimated anthropogenic aerosol direct radiative forcing over oceans without due consideration of cloudy-sky aerosols. However, when interaction between clouds and aerosols located below or above the cloud level is taken into account, the aerosol direct radiative forcing is larger by as much as 5 W m-2 in most mid-latitude regions in the Northern Hemisphere.

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