Articles | Volume 14, issue 20
https://doi.org/10.5194/acp-14-11287-2014
https://doi.org/10.5194/acp-14-11287-2014
Research article
 | 
27 Oct 2014
Research article |  | 27 Oct 2014

An important mechanism sustaining the atmospheric "water tower" over the Tibetan Plateau

X. Xu, T. Zhao, C. Lu, Y. Guo, B. Chen, R. Liu, Y. Li, and X. Shi

Viewed

Total article views: 5,852 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
3,374 2,351 127 5,852 99 125
  • HTML: 3,374
  • PDF: 2,351
  • XML: 127
  • Total: 5,852
  • BibTeX: 99
  • EndNote: 125
Views and downloads (calculated since 10 Jul 2014)
Cumulative views and downloads (calculated since 10 Jul 2014)

Cited

Saved (final revised paper)

Saved (final revised paper)

Saved (preprint)

Latest update: 13 Dec 2024
Download
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.
Altmetrics
Final-revised paper
Preprint