Articles | Volume 14, issue 20
https://doi.org/10.5194/acp-14-11287-2014
© Author(s) 2014. 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-14-11287-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
An important mechanism sustaining the atmospheric "water tower" over the Tibetan Plateau
X. Xu
State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing, 100081, China
T. Zhao
Key Lab for Aerosol-Cloud-Precipitation of CMA, School of Atmospheric Physics, Nanjing University of Information Science & Technology, Jiangsu, 210044, China
C. Lu
National Science Foundation, Arlington, VA 22230, USA
Y. Guo
State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing, 100081, China
B. Chen
State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing, 100081, China
R. Liu
National Satellite Meteorological Center, China Meteorological Administration, Beijing, 100081, China
Y. Li
Institute of Plateau Meteorology, China Meteorological Administration, Chengdu, 610072, China
X. Shi
State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing, 100081, China
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Latest update: 23 Nov 2024
Short summary
The Tibetan Plateau (TP) with its thermal structure leads to dynamic processes of vapor transport, similar to the CISK mechanism of tropical cyclones.
Two CISK-like processes, contiguous horizontally but staggered vertically, in two ladders over the southern slopes and main platform of the TP relay the moist air over the TP. An integration of mechanical and thermal TP forcing is revealed in relation to the Asian summer monsoon circulation transporting water vapor from tropical oceans to the TP.
The Tibetan Plateau (TP) with its thermal structure leads to dynamic processes of vapor...
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