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昆仑山北坡陆地水储量变化及其驱动因素分析

夏婷婷 薛璇 王灏伟 徐文哲 盛紫怡 汪洋

干旱区地理2024,Vol.47Issue(8):1292-1303,12.
干旱区地理2024,Vol.47Issue(8):1292-1303,12.DOI:10.12118/j.issn.1000-6060.2024.094

昆仑山北坡陆地水储量变化及其驱动因素分析

Changes in terrestrial water storage and its drivers on the north slope of Kunlun Mountains

夏婷婷 1薛璇 2王灏伟 2徐文哲 2盛紫怡 2汪洋1

作者信息

  • 1. 新疆农业大学草业学院,新疆 乌鲁木齐 830052
  • 2. 新疆农业大学资源与环境学院,新疆 乌鲁木齐 830052
  • 折叠

摘要

Abstract

Terrestrial water storage are crucial in the hydrological cycle.Analyzing the dynamics of these re-serves and their main driving mechanisms provides a scientific basis for the macro-control,management,and pro-tection of water resources.This study examines the dynamic changes in terrestrial water storage on the north slope of the Kunlun Mountains from 1990 to 2020,utilizing multi-source data including GRACE data,meteoro-logical data,actual evapotranspiration,and human activities.It quantitatively evaluates the influence of various factors on the long-term changes in water storage in this region.The results indicate significant variation and dif-ferentiation in water reserves across the area.Notably,79.63%of the area showed an increasing trend.Water re-serves in the Yarkant River Basin exhibited deficits,while those in the Kumukuli Basin displayed significant sur-pluses.The overall increase in water reserves on the north slope was 0.123 cm·a-1,with the peak rate occurring in 2005-2006,marking a change of 2.253 cm.The Kumukuli Basin,along with the Keriya River Basin,Qarqan River Basin,and Hotan River Basin,all demonstrated increasing trends,especially notable in the Kumukuli Ba-sin.Both temperature,precipitation and evapotranspiration showed fluctuating upward trends from 1990 to 2020,with average annual precipitation varying significantly and exhibiting spatial heterogeneity.The correlation be-tween terrestrial water storage and average annual temperature,precipitation,and actual evapotranspiration over the 30-year period showed varying degrees of correlation,with positive correlation areas accounting for 40.78%,54.19%,and 44.74%,respectively.Among meteorological factors,temperature and precipitation were the primary drivers of changes in terrestrial water storage.The strongest explanatory power was observed in the interaction be-tween temperature and population density(0.823),and between temperature and precipitation(0.713)among me-teorological factors,indicating that their combined impact significantly exceeds that of any single factor.

关键词

陆地水储量/GRACE/气候变化/人类活动/昆仑山北坡

Key words

terrestrial water storage/GRACE/climate change/human activities/north slope of Kunlun Moun-tains

引用本文复制引用

夏婷婷,薛璇,王灏伟,徐文哲,盛紫怡,汪洋..昆仑山北坡陆地水储量变化及其驱动因素分析[J].干旱区地理,2024,47(8):1292-1303,12.

基金项目

第三次新疆综合科学考察项目(2021xjkk010202)资助 (2021xjkk010202)

干旱区地理

OA北大核心CSTPCD

1000-6060

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