Articles | Volume 15, issue 11
https://doi.org/10.5194/acp-15-6205-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-6205-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Quantifying sources, transport, deposition, and radiative forcing of black carbon over the Himalayas and Tibetan Plateau
R. Zhang
Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000, Gansu, China
Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory (PNNL), Richland, WA 99352, USA
Department of Atmospheric Sciences, Box 351640, University of Washington, Seattle, WA 98195, USA
Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory (PNNL), Richland, WA 99352, USA
Y. Qian
Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory (PNNL), Richland, WA 99352, USA
P. J. Rasch
Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory (PNNL), Richland, WA 99352, USA
R. C. Easter
Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory (PNNL), Richland, WA 99352, USA
Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory (PNNL), Richland, WA 99352, USA
B. Singh
Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory (PNNL), Richland, WA 99352, USA
Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000, Gansu, China
Q. Fu
Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000, Gansu, China
Department of Atmospheric Sciences, Box 351640, University of Washington, Seattle, WA 98195, USA
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- Investigating the relative responses of regional monsoon dynamics to snow darkening and direct radiative effects of dust and carbonaceous aerosols over the Indian subcontinent S. Das et al. 10.1007/s00382-020-05307-1
- Seasonal transition of Black carbon aerosols over Qinghai-Tibet Plateau: Simulations with WRF-Chem Y. Zhou et al. 10.1016/j.atmosenv.2023.119866
- Regional and Sectoral Sources for Black Carbon Over South China in Spring and Their Sensitivity to East Asian Summer Monsoon Onset C. Fang et al. 10.1029/2020JD033219
- Evaluating and Addressing the Leakage Problems of Black Carbon Mitigation in China’s Domestic Sector Y. Xu & J. Liu 10.1021/acs.est.6b02046
- Re-evaluating black carbon in the Himalayas and the Tibetan Plateau: concentrations and deposition C. Li et al. 10.5194/acp-17-11899-2017
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- Direct Radiative Forcing Induced by Light‐Absorbing Aerosols in Different Climate Regions Over East Asia X. Zhang et al. 10.1029/2019JD032228
- Deciphering the Role of Aerosol‐Induced Snow Albedo Feedback on Dust Emission Over the Tibetan Plateau K. Usha et al. 10.1029/2021JD036384
- Fossil Fuel Combustion Emission From South Asia Influences Precipitation Dissolved Organic Carbon Reaching the Remote Tibetan Plateau: Isotopic and Molecular Evidence C. Li et al. 10.1029/2017JD028181
- Importance of local non-fossil sources to carbonaceous aerosols at the eastern fringe of the Tibetan Plateau, China: Δ14C and δ13C evidences C. Li et al. 10.1016/j.envpol.2022.119858
- Modeling the transport of PM10, PM2.5, and O3 from South Asia to the Tibetan Plateau Y. Hu et al. 10.1016/j.atmosres.2024.107323
- Sources of black carbon to the Himalayan–Tibetan Plateau glaciers C. Li et al. 10.1038/ncomms12574
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Short summary
We use the CAM5 model with a novel source-tagging technique to characterize the fate of BC particles emitted from various geographical regions and sectors and their transport pathways to the Himalayas and Tibetan Plateau (HTP). We show a comprehensive picture of the seasonal and regional dependence of BC source attributions, and find strong seasonal and spatial variations in BC-in-snow radiative forcing in the HTP that can be quantitatively attributed to the various regional/sectoral sources.
We use the CAM5 model with a novel source-tagging technique to characterize the fate of BC...
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