中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Increased nonstationarity of stormflow threshold behaviors in a forested watershed due to abrupt earthquake disturbance

文献类型:期刊论文

作者Zhang, Guotao; Cui, Peng; Gualtieri, Carlo; Bazai, Nazir Ahmed; Zhang, Xueqin; Zhang, Zhengtao
刊名HYDROLOGY AND EARTH SYSTEM SCIENCES
出版日期2023-08-14
卷号27期号:15页码:3005-3020
ISSN号1027-5606
DOI10.5194/hess-27-3005-2023
产权排序1
文献子类Article
英文摘要Extreme earthquake disturbances to the vegetation of local and regional landscapes could swiftly impair the former hydrologic function, significantly increasing the challenge of predicting threshold behaviors of rainfall-runoff processes as well as the hydrologic system's complexity over time. It is still unclear how alternating catchment hydrologic behaviors under an ongoing large earthquake disruption are mediated by long-term interactions between landslides and vegetation evolution. In a well-known watershed affected by the Wenchuan earthquake, the nonlinear hydrologic behavior is examined using two thresholds with intervening linear segments. A lower rising threshold (THr) value (210.48 mm) observed in post-earthquake local landslide regions exhibited a faster stormflow response rate than that in undisturbed forest and grassland-shrubland regions, easily triggering huge flash-flood disasters. Additionally, an integrated response metric pair (integrated watershed average generation threshold THg-IWA and rising threshold THr-IWA) with areas of disparate land use, ecology, and physiography was proposed and efficiently applied to identify emergent catchment hydrologic behaviors. The interannual variation in the two integrated hydrologic thresholds before and following the earthquake was assessed to detect the temporal nonstationarity in hydrologic extremes and nonlinear runoff response. The year 2011 was an important turning point along the hydrologic disturbance-recovery timescale following the earthquake, as post-earthquake landslide evolution reached a state of extreme heterogeneity in space. At that time, the THr-IWA value decreased by similar to 9 mm compared with the pre-earthquake level. This is closely related to the fast expansion of landslides, leading to a larger extension of variable source area from the channel to neighboring hillslopes, and faster subsurface stormflow, contributing to flash floods. Finally, we present a conceptual model interpreting how the short- and long-term interactions between earthquake-induced landslides and vegetation affect flood hydrographs at event timescale that generated an increased nonstationary hydrologic behavior. This study expands our current knowledge of threshold-based hydrologic and nonstationary storm-flow behaviors in response to abrupt earthquake disturbance for the prediction of future flood regimes.
WOS关键词FISSURED GRANITIC CATCHMENT ; WENCHUAN EARTHQUAKE ; RUNOFF RESPONSE ; LANDSLIDES ; CONNECTIVITY ; STREAMFLOW ; RAINFALL ; STORAGE ; FLOOD ; IMPACTS
WOS研究方向Geology ; Water Resources
语种英语
出版者COPERNICUS GESELLSCHAFT MBH
WOS记录号WOS:001048142500001
源URL[http://ir.igsnrr.ac.cn/handle/311030/194519]  
专题陆地表层格局与模拟院重点实验室_外文论文
作者单位1.University of Naples Federico II
2.Beijing Normal University
3.Institute of Geographic Sciences & Natural Resources Research, CAS
4.Chinese Academy of Sciences
推荐引用方式
GB/T 7714
Zhang, Guotao,Cui, Peng,Gualtieri, Carlo,et al. Increased nonstationarity of stormflow threshold behaviors in a forested watershed due to abrupt earthquake disturbance[J]. HYDROLOGY AND EARTH SYSTEM SCIENCES,2023,27(15):3005-3020.
APA Zhang, Guotao,Cui, Peng,Gualtieri, Carlo,Bazai, Nazir Ahmed,Zhang, Xueqin,&Zhang, Zhengtao.(2023).Increased nonstationarity of stormflow threshold behaviors in a forested watershed due to abrupt earthquake disturbance.HYDROLOGY AND EARTH SYSTEM SCIENCES,27(15),3005-3020.
MLA Zhang, Guotao,et al."Increased nonstationarity of stormflow threshold behaviors in a forested watershed due to abrupt earthquake disturbance".HYDROLOGY AND EARTH SYSTEM SCIENCES 27.15(2023):3005-3020.

入库方式: OAI收割

来源:地理科学与资源研究所

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