Articles | Volume 20, issue 3
https://doi.org/10.5194/acp-20-1507-2020
© Author(s) 2020. 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-20-1507-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Modeling dust sources, transport, and radiative effects at different altitudes over the Tibetan Plateau
Zhiyuan Hu
Key Laboratory for Semi-Arid Climate Change of the Ministry of
Education, College of Atmospheric Sciences, Lanzhou University, Lanzhou, China
School of Atmospheric Sciences and Guangdong Province Key Laboratory
for Climate Change and Natural Disaster Studies, Sun Yat-sen University, Zhuhai, China
Key Laboratory for Semi-Arid Climate Change of the Ministry of
Education, College of Atmospheric Sciences, Lanzhou University, Lanzhou, China
Chun Zhao
School of Earth and Space Sciences, University of Science and
Technology of China, Hefei, Anhui, China
Qinjian Jin
Department of Geography and Atmospheric Science, The University of Kansas, Lawrence, KS, USA
Yuanyuan Ma
Key Laboratory of Land Surface Process and Climate Change in Cold and Arid Regions, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, China
Ben Yang
School of Atmospheric Sciences, Nanjing University, Nanjing, China
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Latest update: 23 Nov 2024
Short summary
This study investigates intercontinental transport of dust plums and distribution characteristics of dust at different altitudes over the Tibetan Plateau (TP). The results show that dust particles are emitted into atmosphere and then transport to the TP. The East Asian dust trasnports southward and is lifted up to the TP in northern slop, while the North Afican dust and Middle East dust transport eastward and concentrate in both northern and southern slops, then is lifted up to the TP.
This study investigates intercontinental transport of dust plums and distribution...
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