Department of Lower Atmosphere Observation Research (LAOR), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
College of Earth and Planetary Science, University of Chinese Academy of Sciences, Beijing, China
State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
College of Earth and Planetary Science, University of Chinese Academy of Sciences, Beijing, China
State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
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1,959
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2,477
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Supplement: 120
BibTeX: 89
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398
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Total article views: 3,066 (including HTML, PDF, and XML)
Thereof 3,063 with geography defined
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Total article views: 2,477 (including HTML, PDF, and XML)
Thereof 2,477 with geography defined
and 0 with unknown origin.
Total article views: 589 (including HTML, PDF, and XML)
Thereof 586 with geography defined
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By integrating the SNICAR model with Polar-WRF, we find that 50 ng g−1 black carbon (BC) deposition decreases snow albedo, increasing radiative forcing (RF) by 1–4 W m−2, especially in Greenland, Baffin Island, and eastern Siberia. The impact is strongly linked to BC mass, with deep snowpacks showing greater sensitivity. Snowmelt and land–atmosphere interactions are crucial. High-resolution modelling is necessary to better understand these effects on Arctic climate change.
By integrating the SNICAR model with Polar-WRF, we find that 50 ng g−1 black carbon (BC)...
