干旱区研究

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2021 , Vol. 38 >Issue 3: 618 - 628

DOI: https://doi.org/10.13866/j.azr.2021.03.04

水资源及其利用

念青唐古拉山西段冰湖时空变化分析

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  • 1.首都师范大学资源环境与旅游学院,北京 100048
    2.中国地质大学（武汉）地理与信息工程学院,湖北 武汉 430074
    3.深圳市龙华区发展研究院,广东 深圳 518110
陶静（1997-）,女,硕士研究生,主要从事资源环境遥感研究. E-mail: jingt_yeol@l63.com

收稿日期: 2020-07-29

  修回日期: 2020-09-16

  网络出版日期: 2021-06-17

基金资助

国家自然基金项目(41971381);北京水务局重点项目(TAHP-2018-ZB-YY-490S);中央高校基金资助项目(CUG160818)

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Spatial changes of the glacial lakes in the western Nyainqentanglha Range

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  • 1. College of Resources Environment and Tourism, Capital Normal University, Beijing 100048, China
    2. School of Geography and Information Engineering, China University of Geosciences, Wuhan 430074, Hubei, China
    3. Shenzhen Longhua District Development Research Institute, Shenzhen 518110, Guangdong, China

Received date: 2020-07-29

  Revised date: 2020-09-16

  Online published: 2021-06-17

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摘要

基于多源、多期遥感影像与DEM提取的冰湖数据,分析了念青唐古拉山西段1991—2017年冰湖不同维度的分布变化,在此基础上研究了冰湖数量、面积变化与气温、降水变化的关系。结果表明:（1） 近年来,研究区的冰湖数量与面积均呈上升趋势,冰湖数量增加161个,面积增加1.185 km2。其中,1991—2006年平稳增长,2006—2017年大幅增长。（2） 冰湖面积与数量在中高海拔范围内均呈增长趋势。新增冰湖主要分布在海拔5400~5700 m,冰湖数量占整体数量的72.41%。（3） 分布在不同朝向冰湖的增长速率不同。西南向冰湖增长较为迅速,朝北向冰湖增长相对缓慢。（4） 气温上升引起的冰川消融是冰湖生长的间接因素,降水是冰湖生长的重要因素。面积小的冰湖对气候的响应更灵敏,变化更显著,面积大的冰湖,变化幅度小,表明冰湖的动态变化与气候变化紧密相关。通过探究念青唐古拉山西段冰湖变化对冰湖溃决灾害的预测具有重要的指示意义。

关键词： 念青唐古拉山西段; 遥感; 冰湖; 气候变化

本文引用格式

陶静,赵文吉,王旭,薛进 . 念青唐古拉山西段冰湖时空变化分析[J]. 干旱区研究, 2021 , 38(3) : 618 -628 . DOI: 10.13866/j.azr.2021.03.04

Abstract

Based on the multi-source remote sensing image and DEM data, we analyzed the distribution and analysis of different dimensions of glacial lakes in western Nyainqentanglha from 1991 to 2017. Then we analyzed the relationship between changes in ice lakes and temperature and precipitation. The research results showed that the number and area of ice lakes in the study area had increased recently. They increased steadily from 1991 to 2006 and expanded from 2006 to 2107. The number of ice lakes increased by 161, and the area by 1.185 km2 in 26 years. The area and number of ice lakes are increasing in the middle-and high-altitude range. The newly-added ice lakes are mainly 5400-5700 m above sea level, and the number of ice lakes accounts for 72.41% of the total number. The distribution and growth rates of glacial lakes with different aspects are different. The glacial lake on the southwest slope grew rapidly, while the north slope’s glacial lake grew slowly. Glacier melting caused by rising temperatures is an indirect factor for ice lake growth, and precipitation is an essential factor for ice lake growth. Ice lakes with smaller area grades have a more sensitive response to climate and more significant changes. Ice lakes with larger area grades have stronger stability and smaller changes. The dynamic change of ice lakes is closely related to climate change, and it is instructive for predicting glaciers change and ice lake collapse disasters in western Nyainqentanglha.

Key words： western Nyainqentanglha Range; remote sensing; glacial lake; climate change

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