Bimodal hydrographs in a semi-humid forested watershed: characteristics and occurrence conditions
Abstract P mm; (2) isotopic hydrograph separation reveals that the delayed stormflow process is primarily driven by pre-event water, with increasing contributions of pre-event water during catchment wetting up; and (3) the dynamic variation in groundwater level precedes that of streamflow, establishing a hysteretic relationship wherein the groundwater level peaks before streamflow during delayed stormflow. These findings, supported by on-site observations, emphasize the dominance of shallow groundwater flow in the generation of delayed stormflow.
- Standort
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Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
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Online-Ressource
- Sprache
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Englisch
- Erschienen in
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Bimodal hydrographs in a semi-humid forested watershed: characteristics and occurrence conditions ; volume:28 ; number:15 ; year:2024 ; pages:3613-3632 ; extent:20
Hydrology and earth system sciences ; 28, Heft 15 (2024), 3613-3632 (gesamt 20)
- Urheber
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Cui, Zhen
Tian, Fuqiang
Zhao, Zilong
Xu, Zitong
Duan, Yongjie
Wen, Jie
Khan, Mohd Yawar Ali
- DOI
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10.5194/hess-28-3613-2024
- URN
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urn:nbn:de:101:1-2408150434172.471223083290
- Rechteinformation
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
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14.08.2025, 10:51 MESZ
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Beteiligte
- Cui, Zhen
- Tian, Fuqiang
- Zhao, Zilong
- Xu, Zitong
- Duan, Yongjie
- Wen, Jie
- Khan, Mohd Yawar Ali
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