干旱区科学2024,Vol.16Issue(7) :877-894.DOI:10.1007/s40333-024-0080-5

Glacier area change and its impact on runoff in the Manas River Basin,Northwest China from 2000 to 2020

WANG Tongxia CHEN Fulong LONG Aihua ZHANG Zhengyong HE Chaofei LYU Tingbo LIU Bo HUANG Yanhao
干旱区科学2024,Vol.16Issue(7) :877-894.DOI:10.1007/s40333-024-0080-5

Glacier area change and its impact on runoff in the Manas River Basin,Northwest China from 2000 to 2020

WANG Tongxia 1CHEN Fulong 1LONG Aihua 2ZHANG Zhengyong 3HE Chaofei 4LYU Tingbo 4LIU Bo 4HUANG Yanhao4
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作者信息

  • 1. College of Water Conservancy&Architectural Engineering,Shihezi University,Shihezi 832000,China;Key Laboratory of Cold and Arid Regions Eco-Hydraulic Engineering of Xinjiang Production&Construction Corps,Shihezi 832000,China
  • 2. College of Water Conservancy&Architectural Engineering,Shihezi University,Shihezi 832000,China;State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin,China Institute of Water Resources and Hydropower Research,Beijing 100038,China
  • 3. College of Sciences,Shihezi University,Shihezi 832000,China
  • 4. College of Water Conservancy&Architectural Engineering,Shihezi University,Shihezi 832000,China
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Abstract

Understanding the distribution and dynamics of glaciers is of great significance to the management and allocation of regional water resources and socio-economic development in arid regions of Northwest China.In this study,based on 36 Landsat images,we extracted the glacier boundaries in the Manas River Basin,Northwest China from 2000 to 2020 using eCognition combined with band operation,GIS(geographic information system)spatial overlay techniques,and manual visual interpretation.We further analyzed the distribution and variation characteristics of glacier area,and simulated glacial runoff using a distributed degree-day model to explore the regulation of runoff recharge.The results showed that glacier area in the Manas River Basin as a whole showed a downward trend over the past 21 a,with a decrease of 10.86%and an average change rate of-0.54%/a.With the increase in glacier scale,the number of smaller glaciers decreased exponentially,and the number and area of larger glaciers were relatively stable.Glacier area showed a normal distribution trend of increasing first and then decreasing with elevation.About 97.92%of glaciers were distributed at 3700-4800 m,and 48.11%of glaciers were observed on the northern and northeastern slopes.The retreat rate of glaciers was the fastest(68.82%)at elevations below 3800 m.There was a clear rise in elevation at the end of glaciers.Glaciers at different slope directions showed a rapid melting trend from the western slope to the southern slope then to the northern slope.Glacial runoff in the basin showed a fluctuating upward trend in the past 21 a,with an increase rate of 0.03×108 m3/a.The average annual glacial runoff was 4.80×108 m3,of which 33.31%was distributed in the ablation season(June-September).The average annual contribution rate of glacial meltwater to river runoff was 35.40%,and glacial runoff accounted for 45.37%of the total runoff during the ablation season.In addition,precipitation and glacial runoff had complementary regulation patterns for river runoff.The findings can provide a scientific basis for water resource management in the Manas River Basin and other similar arid inland river basins.

Key words

glacier area/glacial runoff/climate change/glacier boundary extraction/distributed degree-day model/Manas River Basin

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基金项目

National Natural Science Foundation of China(52169005)

Support Plan for Innovation and Development of Key Industries in southern Xinjiang,China(2022DB024)

Corps Science and Technology Innovation Talents Program Project of China(2023CB008-08)

出版年

2024
干旱区科学
中国科学院新疆生态与地理研究所,科学出版社

干旱区科学

CSTPCDCSCD
影响因子:1.743
ISSN:1674-6767
参考文献量2
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