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1000 Titel
  • Spatiotemporal responses of runoff to climate change in the southern Tibetan Plateau
1000 Autor/in
  1. Sun, HE |
  2. Yao, Tandong |
  3. Su, Fengge |
  4. Yang, Wei |
  5. Chen, Deliang |
1000 Verlag Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-09-25
1000 Erschienen in
1000 Quellenangabe
  • 28(18):4361-4381
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/hess-28-4361-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. A comprehensive understanding of spatiotemporal runoff changes in the Yarlung Zangbo (YZ) basin in the southern Tibetan Plateau (TP) at a sub-basin scale, amidst varying climatic and cryospheric conditions, is imperative for effective water resources management. However, spatiotemporal differences of runoff composition and change and their attribution within the YZ basin have not been extensively explored, primarily due to the lack of hydrometeorological observations, especially in the downstream region. In this study, we investigated historical and future evolution of annual and seasonal total water availability, as well as glacier runoff and snowmelt contributions across six sub-basins of the YZ, with a particular focus on the comparison between the upstream Nuxia (NX) basin and the downstream Nuxia–Pasighat (NX-BXK) basin, based on a newly generated precipitation dataset and a well-validated model with streamflow, glacier mass, and snow cover observations. Our findings revealed that large spatiotemporal differences in changes exist within the YZ basin for 1971–2020. Firstly, runoff generation was dominated by rainfall runoff throughout the YZ basin, with glacier runoff playing a more important role in the annual total runoff (19 %) in the NX-BXK sub-basin compared to other sub-basins. Notably, glacier runoff contributed 52 % of the total runoff at the Pasighat outlet of the YZ basin. Secondly, annual runoff exhibited an increasing trend in the NX basin but a decreasing trend in the NX-BXK, primarily attributed to rainfall runoff changes influenced by atmospheric moisture. Glacier runoff enhanced water supply by offsetting the decreasing contribution from rainfall. Total runoff will consistently increase (27–100 mm (10 yr)−1) across the sub-basins through the 21st century, resulting from increased rainfall runoff and a minor effect of increased snowmelt and glacier runoff. </jats:p>
1000 Fächerklassifikation (DDC)
1000 Liste der Beteiligten
  1. https://orcid.org/0000-0001-8305-9507|https://frl.publisso.de/adhoc/uri/WWFvLCBUYW5kb25n|https://frl.publisso.de/adhoc/uri/U3UsIEZlbmdnZQ==|https://frl.publisso.de/adhoc/uri/WWFuZywgV2Vp|https://orcid.org/0000-0003-0288-5618
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1000 Label
1000 Förderer
  1. National Natural Science Foundation of China |
  2. China Postdoctoral Science Foundation |
1000 Fördernummer
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  2. -
1000 Förderprogramm
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  2. -
1000 Dateien
1000 Förderung
  1. 1000 joinedFunding-child
    1000 Förderer National Natural Science Foundation of China |
    1000 Förderprogramm -
    1000 Fördernummer -
  2. 1000 joinedFunding-child
    1000 Förderer China Postdoctoral Science Foundation |
    1000 Förderprogramm -
    1000 Fördernummer -
1000 Objektart article
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1000 @id frl:6487003.rdf
1000 Erstellt am 2024-10-03T04:36:42.042+0200
1000 Erstellt von 322
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1000 Zuletzt bearbeitet 2025-08-13T23:55:58.671+0200
1000 Objekt bearb. Wed Aug 13 23:55:58 CEST 2025
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