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DOI | 10.1016/j.atmosres.2019.07.001 |
Empirical evidence of a positive climate forcing of aerosols at elevated albedo | |
Yoon J.; Chang D.Y.; Lelieveld J.; Pozzer A.; Kim J.; Yum S.S. | |
发表日期 | 2019 |
ISSN | 0169-8095 |
起始页码 | 269 |
结束页码 | 279 |
卷号 | 229 |
英文摘要 | We use Aerosol Robotic Network (AERONET) observation data to empirically determine how natural and anthropogenic aerosol categories (i.e. mineral dust, biomass burning, and urban-industrial aerosols) affect light extinction, showing that their radiative forcing varies strongly with the surface albedo. Generally, the radiative forcing depends on the aerosol loading, but the efficiency varies with the aerosol type and aerosol-radiation-surface interactions. Desert dust, biomass burning and urban-industrial aerosols can exhibit dramatic shifts in radiative forcing at the top of the atmosphere, from cooling to warming, at surface albedos from below 0.5 to above 0.75. Based on the linear relationship between the radiative forcing efficiency and surface albedo for aeolian aerosols, using Moderate Resolution Imaging Spectroradiometer (MODIS) AOT (Aerosol Optical Thickness) and surface albedo data, we characterized a large Asian dust event during the spring of 2001, and demonstrate its immense spatially varying radiative forcing, ranging from about −84.0 to +69.3 W/m2. For extensive Russian wildfires during the summer of 2010, strong radiative cooling forcing variability of biomass combustion aerosols is found, ranging from about −86.3 to +3.1 W/m2. For a thick urban-industrial aerosol haze over northern India during the winter of 2017, a large range of about −85.0 to −0.3 W/m2 is found. These wide ranges underscore the need to accurately define aerosol-radiation-surface interactions. © 2019 The Authors |
英文关键词 | AERONET; Aerosol optical thickness; Aerosol radiative effects; Aerosol-radiation-surface interactions; MODIS; Surface albedo |
语种 | 英语 |
scopus关键词 | Atmospheric radiation; Biomass; Combustion; Dust; Efficiency; Light extinction; Optical properties; Radiation effects; Radiative Cooling; Radiometers; Solar radiation; AERONET; Aerosol optical thickness; Aerosol radiation; MODIS; Radiative effects; Surface albedo; Aerosols; AERONET; aerosol; albedo; climate forcing; concentration (composition); empirical analysis; MODIS; optical depth; radiative forcing; radiative transfer |
来源期刊 | Atmospheric Research |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/162320 |
作者单位 | Environmental Satellite Center, Climate and Air Quality Research Department, National Institute of Environmental Research, Incheon, 22689, South Korea; Atmospheric Chemistry Department, Max-Planck Institute for Chemistry, P. O. Box 3060, Mainz, 55128, Germany; Department of Atmosphere Sciences, Yonsei University, Seoul, South Korea; The Cyprus Institute, P. O. Box 27456, Nicosia, 1645, Cyprus |
推荐引用方式 GB/T 7714 | Yoon J.,Chang D.Y.,Lelieveld J.,et al. Empirical evidence of a positive climate forcing of aerosols at elevated albedo[J],2019,229. |
APA | Yoon J.,Chang D.Y.,Lelieveld J.,Pozzer A.,Kim J.,&Yum S.S..(2019).Empirical evidence of a positive climate forcing of aerosols at elevated albedo.Atmospheric Research,229. |
MLA | Yoon J.,et al."Empirical evidence of a positive climate forcing of aerosols at elevated albedo".Atmospheric Research 229(2019). |
条目包含的文件 | 条目无相关文件。 |
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