Haiting Zhang , Min Xu , Shichang Kang , Xingdong Li
{"title":"中巴经济走廊融雪洪水变化及驱动因素分析","authors":"Haiting Zhang , Min Xu , Shichang Kang , Xingdong Li","doi":"10.1016/j.jhydrol.2025.133443","DOIUrl":null,"url":null,"abstract":"<div><div>Flooding is one of the most frequent disasters in the China-Pakistan Economic Corridor (CPEC), which is highly dangerous and destructive, and seriously hinders regional socio-economic development. In this study, the Block Maximum (BM) model and the Peak Over Threshold (POT) model were used to analyze the spatial and temporal characteristics of snowmelt floods in the Kashgar River Basin and the Indus River Basin of CPEC during 1948–2022. Historical floods were classified based on principal component analysis and the k-means clustering algorithm. The main climatic factors of snowmelt floods were analyzed using Spearman’s rank correlation coefficient and random forest model. The results indicated that 85 and 93 snowmelt flood events occurred respectively in the two basins, mainly in spring (March–May). The occurrence of snowmelt floods was advanced in the Kashgar River Basin, while that in the Indus River Basin was delayed. Five and four flood classes were identified in the Kashgar River Basin and the Indus River Basin, respectively. Attribution analysis suggested that the snow factors are key preconditions, especially the 14-day antecedent maximum SWE (MSWE). The Kashgar River Basin was more sensitive to 7-day cumulative precipitation (CPr7) from 1982 to 1999, but to 7-day cumulative daily average temperature (TEMP7) from 2000 to 2020. The Indus River Basin was more sensitive to 1-day cumulative precipitation (CPr1) from 1982 to 1999. However, the impact of CPr7 on snowmelt floods increased from 2000 to 2020. The study provides scientific and technological support for snowmelt flood forecasting and prevention in CPEC and regional disaster prevention and mitigation efforts.</div></div>","PeriodicalId":362,"journal":{"name":"Journal of Hydrology","volume":"660 ","pages":"Article 133443"},"PeriodicalIF":5.9000,"publicationDate":"2025-05-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Changes in snowmelt flooding and driver factors in the China-Pakistan Economic Corridor\",\"authors\":\"Haiting Zhang , Min Xu , Shichang Kang , Xingdong Li\",\"doi\":\"10.1016/j.jhydrol.2025.133443\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Flooding is one of the most frequent disasters in the China-Pakistan Economic Corridor (CPEC), which is highly dangerous and destructive, and seriously hinders regional socio-economic development. In this study, the Block Maximum (BM) model and the Peak Over Threshold (POT) model were used to analyze the spatial and temporal characteristics of snowmelt floods in the Kashgar River Basin and the Indus River Basin of CPEC during 1948–2022. Historical floods were classified based on principal component analysis and the k-means clustering algorithm. The main climatic factors of snowmelt floods were analyzed using Spearman’s rank correlation coefficient and random forest model. The results indicated that 85 and 93 snowmelt flood events occurred respectively in the two basins, mainly in spring (March–May). The occurrence of snowmelt floods was advanced in the Kashgar River Basin, while that in the Indus River Basin was delayed. Five and four flood classes were identified in the Kashgar River Basin and the Indus River Basin, respectively. Attribution analysis suggested that the snow factors are key preconditions, especially the 14-day antecedent maximum SWE (MSWE). The Kashgar River Basin was more sensitive to 7-day cumulative precipitation (CPr7) from 1982 to 1999, but to 7-day cumulative daily average temperature (TEMP7) from 2000 to 2020. The Indus River Basin was more sensitive to 1-day cumulative precipitation (CPr1) from 1982 to 1999. However, the impact of CPr7 on snowmelt floods increased from 2000 to 2020. The study provides scientific and technological support for snowmelt flood forecasting and prevention in CPEC and regional disaster prevention and mitigation efforts.</div></div>\",\"PeriodicalId\":362,\"journal\":{\"name\":\"Journal of Hydrology\",\"volume\":\"660 \",\"pages\":\"Article 133443\"},\"PeriodicalIF\":5.9000,\"publicationDate\":\"2025-05-05\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Hydrology\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0022169425007814\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"ENGINEERING, CIVIL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Hydrology","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0022169425007814","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ENGINEERING, CIVIL","Score":null,"Total":0}
Changes in snowmelt flooding and driver factors in the China-Pakistan Economic Corridor
Flooding is one of the most frequent disasters in the China-Pakistan Economic Corridor (CPEC), which is highly dangerous and destructive, and seriously hinders regional socio-economic development. In this study, the Block Maximum (BM) model and the Peak Over Threshold (POT) model were used to analyze the spatial and temporal characteristics of snowmelt floods in the Kashgar River Basin and the Indus River Basin of CPEC during 1948–2022. Historical floods were classified based on principal component analysis and the k-means clustering algorithm. The main climatic factors of snowmelt floods were analyzed using Spearman’s rank correlation coefficient and random forest model. The results indicated that 85 and 93 snowmelt flood events occurred respectively in the two basins, mainly in spring (March–May). The occurrence of snowmelt floods was advanced in the Kashgar River Basin, while that in the Indus River Basin was delayed. Five and four flood classes were identified in the Kashgar River Basin and the Indus River Basin, respectively. Attribution analysis suggested that the snow factors are key preconditions, especially the 14-day antecedent maximum SWE (MSWE). The Kashgar River Basin was more sensitive to 7-day cumulative precipitation (CPr7) from 1982 to 1999, but to 7-day cumulative daily average temperature (TEMP7) from 2000 to 2020. The Indus River Basin was more sensitive to 1-day cumulative precipitation (CPr1) from 1982 to 1999. However, the impact of CPr7 on snowmelt floods increased from 2000 to 2020. The study provides scientific and technological support for snowmelt flood forecasting and prevention in CPEC and regional disaster prevention and mitigation efforts.
期刊介绍:
The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.