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...

Full description

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/10.18452/25424
https://doi.org/10.1029/2022EA002318
_version_ 1829312661892890624
author Guan, Xuefeng
Langhamer, Lukas
Schneider, Christoph
author_facet Guan, Xuefeng
Langhamer, Lukas
Schneider, Christoph
author_sort Guan, Xuefeng
collection Open-Access-Publikationsserver der Humboldt-Universität: edoc-Server
container_issue 7
container_title Earth and Space Science
container_volume 9
description 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
format Article in Journal/Newspaper
genre North Atlantic
Siberia
genre_facet North Atlantic
Siberia
id fthuberlin:oai:edoc.hu-berlin.de:18452/26115
institution Open Polar
language English
op_collection_id fthuberlin
op_doi https://doi.org/10.18452/2542410.1029/2022EA002318
op_relation https://doi.org/10.18452/25424
doi:10.1029/2022EA002318
op_rights (CC BY 4.0) Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/
publishDate 2022
publisher Humboldt-Universität zu Berlin
record_format openpolar
spelling fthuberlin:oai:edoc.hu-berlin.de:18452/26115 2025-04-13T14:23:58+00:00 Lagrangian Analysis of Moisture Sources of Precipitation in the Tianshan Mountains, Central Asia Guan, Xuefeng Langhamer, Lukas Schneider, Christoph 2022-06-24 application/pdf http://edoc.hu-berlin.de/18452/26115 https://nbn-resolving.org/urn:nbn:de:kobv:11-110-18452/26115-4 https://doi.org/10.18452/25424 https://doi.org/10.1029/2022EA002318 eng eng Humboldt-Universität zu Berlin https://doi.org/10.18452/25424 doi:10.1029/2022EA002318 (CC BY 4.0) Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ 550 Geowissenschaften ddc:550 article doc-type:article publishedVersion 2022 fthuberlin https://doi.org/10.18452/2542410.1029/2022EA002318 2025-03-17T04:52:51Z 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 Article in Journal/Newspaper North Atlantic Siberia Open-Access-Publikationsserver der Humboldt-Universität: edoc-Server Earth and Space Science 9 7
spellingShingle 550 Geowissenschaften
ddc:550
Guan, Xuefeng
Langhamer, Lukas
Schneider, Christoph
Lagrangian Analysis of Moisture Sources of Precipitation in the Tianshan Mountains, Central Asia
title Lagrangian Analysis of Moisture Sources of Precipitation in the Tianshan Mountains, Central Asia
title_full Lagrangian Analysis of Moisture Sources of Precipitation in the Tianshan Mountains, Central Asia
title_fullStr Lagrangian Analysis of Moisture Sources of Precipitation in the Tianshan Mountains, Central Asia
title_full_unstemmed Lagrangian Analysis of Moisture Sources of Precipitation in the Tianshan Mountains, Central Asia
title_short Lagrangian Analysis of Moisture Sources of Precipitation in the Tianshan Mountains, Central Asia
title_sort lagrangian analysis of moisture sources of precipitation in the tianshan mountains, central asia
topic 550 Geowissenschaften
ddc:550
topic_facet 550 Geowissenschaften
ddc:550
url http://edoc.hu-berlin.de/18452/26115
https://nbn-resolving.org/urn:nbn:de:kobv:11-110-18452/26115-4
https://doi.org/10.18452/25424
https://doi.org/10.1029/2022EA002318