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Earth System Dynamics An interactive open-access journal of the European Geosciences Union
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Volume 6, issue 1
Earth Syst. Dynam., 6, 109–124, 2015
https://doi.org/10.5194/esd-6-109-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Earth Syst. Dynam., 6, 109–124, 2015
https://doi.org/10.5194/esd-6-109-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 13 Mar 2015

Research article | 13 Mar 2015

A 12-year high-resolution climatology of atmospheric water transport over the Tibetan Plateau

J. Curio1, F. Maussion1,2, and D. Scherer1 J. Curio et al.
  • 1Chair of Climatology, Technische Universität Berlin, Berlin, Germany
  • 2Institute of Meteorology and Geophysics, University of Innsbruck, Innsbruck, Austria

Abstract. The Tibetan Plateau (TP) plays a key role in the water cycle of high Asia and its downstream regions. The respective influence of the Indian and East Asian summer monsoon on TP precipitation and regional water resources, together with the detection of moisture transport pathways and source regions are the subject of recent research. In this study, we present a 12-year high-resolution climatology of the atmospheric water transport (AWT) over and towards the TP using a new data set, the High Asia Refined analysis (HAR), which better represents the complex topography of the TP and surrounding high mountain ranges than coarse-resolution data sets. We focus on spatiotemporal patterns, vertical distribution and transport through the TP boundaries. The results show that the mid-latitude westerlies have a higher share in summertime AWT over the TP than assumed so far. Water vapour (WV) transport constitutes the main part, whereby transport of water as cloud particles (CP) also plays a role in winter in the Karakoram and western Himalayan regions. High mountain valleys in the Himalayas facilitate AWT from the south, whereas the high mountain regions inhibit AWT to a large extent and limit the influence of the Indian summer monsoon. No transport from the East Asian monsoon to the TP could be detected. Our results show that 36.8 ± 6.3% of the atmospheric moisture needed for precipitation comes from outside the TP, while the remaining 63.2% is provided by local moisture recycling.

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