College of Global Change and Earth System Science, State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875, China
Joint Center for Global Change Studies, Beijing Normal University, Beijing 100875, China
College of Global Change and Earth System Science, State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875, China
Joint Center for Global Change Studies, Beijing Normal University, Beijing 100875, China
Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences (CAS), Beijing, 100101, China
Xingchuan Yang
College of Global Change and Earth System Science, State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875, China
Joint Center for Global Change Studies, Beijing Normal University, Beijing 100875, China
College of Global Change and Earth System Science, State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875, China
Joint Center for Global Change Studies, Beijing Normal University, Beijing 100875, China
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EndNote: 197
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Total article views: 3,859 (including HTML, PDF, and XML)
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2,785
973
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3,859
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170
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Total article views: 4,288 (including HTML, PDF, and XML)
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Total article views: 429 (including HTML, PDF, and XML)
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The occurrence frequency of different aerosol types and aerosol optical depth over the Arctic, Antarctic and Tibetan Plateau (TP) show distinctive spatiotemporal differences. The aerosol extinction coefficient in the Arctic and TP has a broad vertical distribution, while that of the Antarctic has obvious seasonal differences. Compared with the Antarctic, the Arctic and TP are vulnerable to surrounding pollutants, and the source of air masses has obvious seasonal variations.
The occurrence frequency of different aerosol types and aerosol optical depth over the Arctic,...
