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
Viewed
Total article views: 1,859 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,497
215
147
1,859
96
55
77
HTML: 1,497
PDF: 215
XML: 147
Total: 1,859
Supplement: 96
BibTeX: 55
EndNote: 77
Views and downloads (calculated since 24 Jun 2024)
Cumulative views and downloads
(calculated since 24 Jun 2024)
Total article views: 1,273 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,099
146
28
1,273
62
44
66
HTML: 1,099
PDF: 146
XML: 28
Total: 1,273
Supplement: 62
BibTeX: 44
EndNote: 66
Views and downloads (calculated since 03 Jan 2025)
Cumulative views and downloads
(calculated since 03 Jan 2025)
Total article views: 586 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
398
69
119
586
34
11
11
HTML: 398
PDF: 69
XML: 119
Total: 586
Supplement: 34
BibTeX: 11
EndNote: 11
Views and downloads (calculated since 24 Jun 2024)
Cumulative views and downloads
(calculated since 24 Jun 2024)
Viewed (geographical distribution)
Total article views: 1,859 (including HTML, PDF, and XML)
Thereof 1,859 with geography defined
and 0 with unknown origin.
Total article views: 1,273 (including HTML, PDF, and XML)
Thereof 1,273 with geography defined
and 0 with unknown origin.
Total article views: 586 (including HTML, PDF, and XML)
Thereof 583 with geography defined
and 3 with unknown origin.
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)...