Effect of Moisture Sources on the Isotopic Composition of Precipitation in Northwest China

Stable isotopes (18O/16O and 2H/1H) are fingerprints of water molecules and thus can be used to gain insight on water circulation. Especially, the factors controlling the isotopic composition of precipitation should be identified because they act as baseline determinants of the isotopic variations o...

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Published in:Water
Main Authors: Yanlong Kong, Ke Wang, Sheng Pan, Yaqian Ren, Weizun Zhang
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/w15081584
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spelling ftmdpi:oai:mdpi.com:/2073-4441/15/8/1584/ 2023-08-20T04:04:41+02:00 Effect of Moisture Sources on the Isotopic Composition of Precipitation in Northwest China Yanlong Kong Ke Wang Sheng Pan Yaqian Ren Weizun Zhang agris 2023-04-19 application/pdf https://doi.org/10.3390/w15081584 EN eng Multidisciplinary Digital Publishing Institute Hydrology https://dx.doi.org/10.3390/w15081584 https://creativecommons.org/licenses/by/4.0/ Water; Volume 15; Issue 8; Pages: 1584 moisture sources stable isotopes precipitation HYSPLIT Northwest China Text 2023 ftmdpi https://doi.org/10.3390/w15081584 2023-08-01T09:44:54Z Stable isotopes (18O/16O and 2H/1H) are fingerprints of water molecules and thus can be used to gain insight on water circulation. Especially, the factors controlling the isotopic composition of precipitation should be identified because they act as baseline determinants of the isotopic variations of surface water and groundwater. Here, using the HYSPLIT model, we attribute observed isotope variations to different moisture sources and characterize the isotopic composition of meteoric precipitation in Northwest China. Results show that the westerlies play a dominant role across the region throughout the year, while other moisture sources only affect some parts of the region during a specific season, i.e., Arctic airflow only affects the Altay Mountains as far as the Middle Tianshan Mountains; the East Asia Monsoon only affects the region east of 100° E longitude during the summer; and summer rainfall of local origin may contribute to the precipitation budget of basin areas. Given the different moisture sources across Northwest China, a local meteoric water line (NWMWL) of δ2H = 6.8δ18O − 1.6 is observed. Our findings not only can provide valuable insights into the mechanism of precipitation isotope fractionation in Northwest China but also can contribute to a better understanding of regional climate and hydrological studies. Text Arctic MDPI Open Access Publishing Arctic Water 15 8 1584
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic moisture sources
stable isotopes
precipitation
HYSPLIT
Northwest China
spellingShingle moisture sources
stable isotopes
precipitation
HYSPLIT
Northwest China
Yanlong Kong
Ke Wang
Sheng Pan
Yaqian Ren
Weizun Zhang
Effect of Moisture Sources on the Isotopic Composition of Precipitation in Northwest China
topic_facet moisture sources
stable isotopes
precipitation
HYSPLIT
Northwest China
description Stable isotopes (18O/16O and 2H/1H) are fingerprints of water molecules and thus can be used to gain insight on water circulation. Especially, the factors controlling the isotopic composition of precipitation should be identified because they act as baseline determinants of the isotopic variations of surface water and groundwater. Here, using the HYSPLIT model, we attribute observed isotope variations to different moisture sources and characterize the isotopic composition of meteoric precipitation in Northwest China. Results show that the westerlies play a dominant role across the region throughout the year, while other moisture sources only affect some parts of the region during a specific season, i.e., Arctic airflow only affects the Altay Mountains as far as the Middle Tianshan Mountains; the East Asia Monsoon only affects the region east of 100° E longitude during the summer; and summer rainfall of local origin may contribute to the precipitation budget of basin areas. Given the different moisture sources across Northwest China, a local meteoric water line (NWMWL) of δ2H = 6.8δ18O − 1.6 is observed. Our findings not only can provide valuable insights into the mechanism of precipitation isotope fractionation in Northwest China but also can contribute to a better understanding of regional climate and hydrological studies.
format Text
author Yanlong Kong
Ke Wang
Sheng Pan
Yaqian Ren
Weizun Zhang
author_facet Yanlong Kong
Ke Wang
Sheng Pan
Yaqian Ren
Weizun Zhang
author_sort Yanlong Kong
title Effect of Moisture Sources on the Isotopic Composition of Precipitation in Northwest China
title_short Effect of Moisture Sources on the Isotopic Composition of Precipitation in Northwest China
title_full Effect of Moisture Sources on the Isotopic Composition of Precipitation in Northwest China
title_fullStr Effect of Moisture Sources on the Isotopic Composition of Precipitation in Northwest China
title_full_unstemmed Effect of Moisture Sources on the Isotopic Composition of Precipitation in Northwest China
title_sort effect of moisture sources on the isotopic composition of precipitation in northwest china
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/w15081584
op_coverage agris
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Water; Volume 15; Issue 8; Pages: 1584
op_relation Hydrology
https://dx.doi.org/10.3390/w15081584
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/w15081584
container_title Water
container_volume 15
container_issue 8
container_start_page 1584
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