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.
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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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)
- Creator
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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
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 10:51 AM CEST
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Associated
- Cui, Zhen
- Tian, Fuqiang
- Zhao, Zilong
- Xu, Zitong
- Duan, Yongjie
- Wen, Jie
- Khan, Mohd Yawar Ali
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Delayed Stormflow Generation in a Semi-humid Forested Watershed Controlled by Soil Water Storage and Groundwater
Developing a representative snow-monitoring network in a forested mountain watershed
Spatial and temporal dynamics of stream chemistry in a forested watershed
Increased carbon capture by a silicate-treated forested watershed affected by acid deposition
Increased carbon capture by a silicate-treated forested watershed affected by acid deposition
Phosphorus fluxes in a temperate forested watershed: canopy leaching, runoff sources, and in-stream transformation
Increased nonstationarity of stormflow threshold behaviors in a forested watershed due to abrupt earthquake disturbance
Increased Nonstationarity of Stormflow Threshold Behaviors in a Forested Watershed Due to Abrupt Earthquake Disturbance
Seasonal patterns in riverine carbon form and export from a temperate forested watershed in Southeast Alaska
Dramatic increase in water use efficiency with cumulative forest disturbance at the large forested watershed scale
The effect of input data complexity on the uncertainty in simulated streamflow in a humid, mountainous watershed
Bimodal Speech Recognition
Delayed Stormflow Generation in a Semi-humid Forested Watershed Controlled by Soil Water Storage and Groundwater
Developing a representative snow-monitoring network in a forested mountain watershed
Spatial and temporal dynamics of stream chemistry in a forested watershed
Increased carbon capture by a silicate-treated forested watershed affected by acid deposition
Increased carbon capture by a silicate-treated forested watershed affected by acid deposition
Phosphorus fluxes in a temperate forested watershed: canopy leaching, runoff sources, and in-stream transformation
Increased nonstationarity of stormflow threshold behaviors in a forested watershed due to abrupt earthquake disturbance
Increased Nonstationarity of Stormflow Threshold Behaviors in a Forested Watershed Due to Abrupt Earthquake Disturbance
Seasonal patterns in riverine carbon form and export from a temperate forested watershed in Southeast Alaska
Dramatic increase in water use efficiency with cumulative forest disturbance at the large forested watershed scale
The effect of input data complexity on the uncertainty in simulated streamflow in a humid, mountainous watershed