Articles | Volume 18, issue 17
https://doi.org/10.5194/acp-18-12683-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-18-12683-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Radiative feedbacks of dust in snow over eastern Asia in CAM4-BAM
SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
Xiaodong Liu
SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
University of Chinese Academy of Sciences, Beijing 100049, China
Huizheng Che
Key Laboratory for Atmospheric Chemistry, Institute of Atmospheric Composition,
Chinese Academy of Meteorological Sciences, CMA, Beijing 100081, China
Xiaoxun Xie
SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
Xinzhou Li
SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
Zhengguo Shi
SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
Hongli Wang
Shaanxi Radio and TV University, Xi'an 710119, China
Tianliang Zhao
Key Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration,
Nanjing University of Science Information & Technology, Nanjing 210044, China
Yangang Liu
Environmental and Climate Sciences Department, Brookhaven National Laboratory, Upton, NY 11973-5000, USA
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Cited
13 citations as recorded by crossref.
- Black carbon and mineral dust in snow cover across a typical city of Northeast China F. Zhang et al. 10.1016/j.scitotenv.2021.150397
- Effect of dust aerosols on the heat exchange over the Taklimakan Desert Z. Tan et al. 10.1016/j.atmosenv.2022.119058
- Enhanced light absorption and reduced snow albedo due to internally mixed mineral dust in grains of snow T. Shi et al. 10.5194/acp-21-6035-2021
- Variation of the aerosol optical properties and validation of MODIS AOD products over the eastern edge of the Tibetan Plateau based on ground-based remote sensing in 2017 Y. You et al. 10.1016/j.atmosenv.2019.117257
- Effects of dust-in-snow forcing over the Tibetan Plateau on the East Asian dust cycle during the Last Glacial Maximum J. Shen et al. 10.1016/j.palaeo.2019.109442
- Modulation of springtime surface sensible heating over the Tibetan Plateau on the interannual variability of East Asian dust cycle X. Xie et al. 10.5194/acp-20-11143-2020
- Linkage between the absorbing aerosol-induced snow darkening effects over the Himalayas-Tibetan Plateau and the pre-monsoon climate over northern India S. Das et al. 10.1007/s00704-021-03871-y
- Snow-darkening versus direct radiative effects of mineral dust aerosol on the Indian summer monsoon onset: role of temperature change over dust sources Z. Shi et al. 10.5194/acp-19-1605-2019
- Distinct responses of Asian summer monsoon to black carbon aerosols and greenhouse gases X. Xie et al. 10.5194/acp-20-11823-2020
- Influence of Wind Velocity and Soil Size Distribution on Emitted Dust Size Distribution: A Wind Tunnel Study R. Wang et al. 10.1029/2020JD033768
- Global Impact of ENSO on Dust Activities with Emphasis on the Key Region from the Arabian Peninsula to Central Asia Y. Huang et al. 10.1029/2020JD034068
- Modeling Dust Direct Radiative Feedbacks in East Asia During the Last Glacial Maximum X. Cheng et al. 10.3390/atmos10030146
- Direct Radiative Effect (DRE) of Dust Aerosols on West African and East Asian Monsoon: The Role of Ocean‐Atmosphere Interactions A. Wang et al. 10.1029/2021JD035917
13 citations as recorded by crossref.
- Black carbon and mineral dust in snow cover across a typical city of Northeast China F. Zhang et al. 10.1016/j.scitotenv.2021.150397
- Effect of dust aerosols on the heat exchange over the Taklimakan Desert Z. Tan et al. 10.1016/j.atmosenv.2022.119058
- Enhanced light absorption and reduced snow albedo due to internally mixed mineral dust in grains of snow T. Shi et al. 10.5194/acp-21-6035-2021
- Variation of the aerosol optical properties and validation of MODIS AOD products over the eastern edge of the Tibetan Plateau based on ground-based remote sensing in 2017 Y. You et al. 10.1016/j.atmosenv.2019.117257
- Effects of dust-in-snow forcing over the Tibetan Plateau on the East Asian dust cycle during the Last Glacial Maximum J. Shen et al. 10.1016/j.palaeo.2019.109442
- Modulation of springtime surface sensible heating over the Tibetan Plateau on the interannual variability of East Asian dust cycle X. Xie et al. 10.5194/acp-20-11143-2020
- Linkage between the absorbing aerosol-induced snow darkening effects over the Himalayas-Tibetan Plateau and the pre-monsoon climate over northern India S. Das et al. 10.1007/s00704-021-03871-y
- Snow-darkening versus direct radiative effects of mineral dust aerosol on the Indian summer monsoon onset: role of temperature change over dust sources Z. Shi et al. 10.5194/acp-19-1605-2019
- Distinct responses of Asian summer monsoon to black carbon aerosols and greenhouse gases X. Xie et al. 10.5194/acp-20-11823-2020
- Influence of Wind Velocity and Soil Size Distribution on Emitted Dust Size Distribution: A Wind Tunnel Study R. Wang et al. 10.1029/2020JD033768
- Global Impact of ENSO on Dust Activities with Emphasis on the Key Region from the Arabian Peninsula to Central Asia Y. Huang et al. 10.1029/2020JD034068
- Modeling Dust Direct Radiative Feedbacks in East Asia During the Last Glacial Maximum X. Cheng et al. 10.3390/atmos10030146
- Direct Radiative Effect (DRE) of Dust Aerosols on West African and East Asian Monsoon: The Role of Ocean‐Atmosphere Interactions A. Wang et al. 10.1029/2021JD035917
Latest update: 29 May 2023
Short summary
This study extends our previous investigation in dust–radiation interactions to investigate SRF and its feedbacks on the regional climate and the dust cycle over east Asia by use of the CAM4-BAM. Our results show that SRF increases the east Asian dust emissions significantly by 13.7 % in the spring, in contrast to −7.6 % of decreased dust emissions by DRF. Hence, a significant feature of SRF on the Tibetan Plateau can create a positive feedback loop to enhance the dust cycle over east Asia.
This study extends our previous investigation in dust–radiation interactions to investigate SRF...
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