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...
Published in: | Earth and Space Science |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Humboldt-Universität zu Berlin
2022
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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 |
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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 |