中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Morphometry of alluvial fans in an alpine valley basin in southeast Tibet: Spatial heterogeneity, controls, and implications

文献类型:期刊论文

作者Han, Pan1,2; Yu, Guo-An2
刊名CATENA
出版日期2025-03-01
卷号250页码:108799
关键词Alluvial fan Morphometry Spatial heterogeneity Primary processes Parlung Tsangpo Basin
ISSN号0341-8162
DOI10.1016/j.catena.2025.108799
产权排序1
文献子类Article
英文摘要The morphometry of alluvial fans is a fundamental yet significant aspect of understanding fan dynamics and controls, offering potential benefits for fan type discrimination and mitigation of geo-hazards such as flash floods and debris flows. However, alluvial fans in alpine regions have received considerably less attention than their counterparts in non-alpine areas, despite their importance. Using Google Earth Pro, remote sensing images, targeted field surveys, and statistical analysis, we examine the morphometry, spatial heterogeneity along with underlying causes, and primary types (fluvial, debris-flow, and colluvial) of alluvial fans in the Parlung Tsangpo Basin (PTB), a large alpine tributary basin of the Yarlung Tsangpo River (upper Brahmaputra River) characterized by deep valleys in southeastern Tibet, China, based on a dataset of 129 fan samples. Our results reveal that: (1) Significant spatial heterogeneity exists in the morphometry of alluvial fans in the PTB, particularly regarding fan area. (2) Fans exhibiting distinct morphometries correspond to different primary processes (debris flow, fluvial, or colluvial dominated), with varying links to their source basins. (3) Discriminant analysis based on three variables (fan slope, source basin area, and Melton's R) can effectively distinguish between fan types and their primary processes. The development of alluvial fans in the PTB is collectively determined by various allogenic and autogenic factors, with primary processes and tributary-junction effects (distal confinement) acting as the main controls. The primary processes, influenced by regional relief (slope), climate (precipitation and temperature), and sediment supply conditions (volume and caliber), play an essential role in fan development, particularly regarding fan slope. In light of global climate change, new fans have been developing in the basin, while some previously stable fans have entered a new active phase. Consequently, debris flows have become a dominant primary process for alluvial fan development in PTB, driving the evolution of fan morphology.
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WOS关键词DEBRIS-FLOW PROCESSES ; SURFACE-MORPHOLOGY ; DEPOSITIONAL STYLE ; FLUVIAL MEGAFAN ; CLIMATIC-CHANGE ; EVOLUTION ; MOUNTAINS ; ALPS ; HAZARD ; LEVEL
WOS研究方向Geology ; Agriculture ; Water Resources
语种英语
WOS记录号WOS:001425568000001
出版者ELSEVIER
源URL[http://ir.igsnrr.ac.cn/handle/311030/212293]  
专题陆地水循环及地表过程院重点实验室_外文论文
通讯作者Yu, Guo-An
作者单位1.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
2.Chinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China;
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GB/T 7714
Han, Pan,Yu, Guo-An. Morphometry of alluvial fans in an alpine valley basin in southeast Tibet: Spatial heterogeneity, controls, and implications[J]. CATENA,2025,250:108799.
APA Han, Pan,&Yu, Guo-An.(2025).Morphometry of alluvial fans in an alpine valley basin in southeast Tibet: Spatial heterogeneity, controls, and implications.CATENA,250,108799.
MLA Han, Pan,et al."Morphometry of alluvial fans in an alpine valley basin in southeast Tibet: Spatial heterogeneity, controls, and implications".CATENA 250(2025):108799.

入库方式: OAI收割

来源:地理科学与资源研究所

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