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Effect of glaciers on the annual catchment water balance within Budyko framework

作     者:Shi-Wei LIU Xiaoming WANG Lu ZHANG Wei-Ming KONG Hong-Kai GAO Cun-De XIAO Shi-Wei LIU;Xiaoming WANG;Lu ZHANG;Wei-Ming KONG;Hong-Kai GAO;Cun-De XIAO

作者机构:State Key Laboratory of Cryospheric SciencesNorthwest Institute of Eco-Environment and ResourcesChinese Academy of SciencesLanzhou730000China University of Chinese Academy of SciencesBeijing100049China CSIRO Land and WaterCanberraACT 2601Australia Key Laboratory of Geographic Information Science(Ministry of Education)East China Normal UniversityShanghai200241China State Key Laboratory of Earth Surface Processes and Resources EcologyBeijing Normal UniversityBeijing100875China 

出 版 物:《Advances in Climate Change Research》 (气候变化研究进展(英文版))

年 卷 期:2022年第13卷第1期

页      面:51-62页

核心收录:

学科分类:0830[工学-环境科学与工程(可授工学、理学、农学学位)] 07[理学] 0705[理学-地理学] 0706[理学-大气科学] 070501[理学-自然地理学] 

基  金:This study was financially supported by the Second Tibetan Plateau Scientific Expedition and Research Program(STEP)(2019QZKK020805) National Natural Science Foundation of China(41690145) supported by Strategic Priority Research Program of Chinese Academy of Sciences(XDA20100305) CAS Pioneer Hundred Talents Program 

主  题:Budyko framework Glacier Water balance Water resource Runoff elasticity 

摘      要:The effects of catchment characteristics and climate variables on water partitioning into evapotranspiratio n and runoff can be evaluated using the Budyko ***,the influence of glaciers on catchment characteristics within the framework has yet been adequately *** we extend the Budyko framework and apply the elasticity method to examine the effects of glaciers on runoff between 2001 and 2010 in 25 upstream catchments of the Tarim River Basin in western *** consideration of glacier mass balance and glacier fraction improves the performance of the Budyko framework,especially for the catchments with a high glacier *** found that the catchment characteristic parameterwas strongly affected by glacier fraction,and it changes from 1.15 to 2.09 when glacier fraction decreases from 0.4191 to *** also reflects the change in water-energy partitioning that eventually effects on evapotranspiration and *** further assessed the average runoff responses to changes in precipitation,potential evapotranspiration,glacier mass balance,and glacier fraction in the 25 *** the runoff appears most sensitive to precipitation in average,its sensitivity to glacier mass balance and glacier area in fact rises from-0.07%to 0.17% and about 0-0.54%,respectively,when the glacier fraction increases from 0.0005 to 0.4191,further demonstrating the increasing influence of glaciers when the fraction becomes *** all,the inclusion of glacier factors in the Budyko framework allows us to understand more about the impacts and contributions of glaciers to runoff at a catchment scale.

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