Key Laboratory of Tibetan Environment Changes and Land Surface
Processes, Institute of Tibetan Plateau Research, Chinese Academy of
Sciences (CAS), Beijing 100101, China
CAS Center for Excellence in Tibetan Plateau Earth Sciences, Institute
of Tibetan Plateau Research, Chinese Academy of
Sciences (CAS), Beijing 100101, China
School of Earth and Space Sciences, University of Science and
Technology of China, Hefei 230026, China
Shichang Kang
CAS Center for Excellence in Tibetan Plateau Earth Sciences, Institute
of Tibetan Plateau Research, Chinese Academy of
Sciences (CAS), Beijing 100101, China
State Key Laboratory of Cryospheric Sciences, Northwest Institute of
Eco-Environment and Resources, Chinese Academy of
Sciences (CAS), Lanzhou 730000, China
Delong Zhao
Beijing Weather Modification Office, Beijing 100101, China
Yan Yang
Beijing Weather Modification Office, Beijing 100101, China
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Total article views: 4,160 (including HTML, PDF, and XML)
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3,326
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4,160
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PDF: 750
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Supplement: 217
BibTeX: 120
EndNote: 150
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322
1,886
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2,217
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14
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HTML: 322
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Total: 2,217
Supplement: 164
BibTeX: 14
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Total article views: 6,377 (including HTML, PDF, and XML)
Thereof 6,373 with geography defined
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Total article views: 4,160 (including HTML, PDF, and XML)
Thereof 4,160 with geography defined
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Analysis of multiple numerical experiments over the Himalayas and Tibetan Plateau (TP) shows that the complex topography results in 50 % stronger overall cross-Himalayan transport during the pre-monsoon season primarily due to the strengthened efficiency of near-surface meridional transport towards the TP, enhanced wind speed in some valleys and deeper valley channels associated with larger transported BC mass volume, which leads to 30–50 % stronger BC radiative heating over the TP.
Analysis of multiple numerical experiments over the Himalayas and Tibetan Plateau (TP) shows...
