Lagrangian Analysis of Moisture Sources of Precipitation in the Tianshan Mountains, Central Asia

The article processing charge was funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) – 491192747 and the Open Access Publication Fund of Humboldt-Universität zu Berlin. The moisture sources of precipitation in the Tianshan Mountains, one of the regions with the highest p...

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Bibliographic Details
Published in:Earth and Space Science
Main Authors: Guan, Xuefeng, Langhamer, Lukas, Schneider, Christoph
Format: Article in Journal/Newspaper
Language:English
Published: Humboldt-Universität zu Berlin 2022
Subjects:
Online Access:http://edoc.hu-berlin.de/18452/26115
https://nbn-resolving.org/urn:nbn:de:kobv:11-110-18452/26115-4
https://doi.org/10.1029/2022EA002318
https://doi.org/10.18452/25424
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Summary:The article processing charge was funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) – 491192747 and the Open Access Publication Fund of Humboldt-Universität zu Berlin. The moisture sources of precipitation in the Tianshan Mountains, one of the regions with the highest precipitation in Central Asia during 1979–2017 are comprehensively and quantitatively summarized by using a Lagrangian moisture source detection technique. Continental sources provide about 93.2% of the moisture for precipitation in the Tianshan Mountain, while moisture directly from the ocean is very limited, averaging only 6.8%. Central Asia plays a dominant role in providing moisture for all sub‐regions of the Tianshan Mountains. For the Western Tianshan, moisture from April to October comes mainly from Central Asia (41.4%), while moisture from November to March is derived primarily from Western Asia (45.7%). Nearly 13.0% of moisture to precipitation for Eastern Tianshan in summer originates from East and South Asia, and the Siberia region. There is a significant decreasing trend in the moisture contribution of local evaporation and Central Asia in the Eastern Tianshan during winter. The contribution of moisture from Europe to summer precipitation in the Central and Eastern Tianshan and the contribution of the North Atlantic Ocean to summer precipitation in the Northern, Central, and Eastern Tianshan also exhibit a decreasing trend. The largest increase in moisture in Western Tianshan stems from West Asia during extreme winter precipitation months. Europe is also an important contributor to extreme precipitation in the Northern Tianshan. The moisture from East and South Asia and Siberia during extreme precipitation months in both winter and summer is significantly enhanced in the Eastern Tianshan. China Scholarship Council Humboldt‐Universität zu Berlin Peer Reviewed