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1985-2021年青藏高原典型湖泊水文特征及关键影响因素

张嘉琪 张会兰 刘雪妍

水土保持学报2024,Vol.38Issue(3):140-149,10.
水土保持学报2024,Vol.38Issue(3):140-149,10.DOI:10.13870/j.cnki.stbcxb.2024.03.025

1985-2021年青藏高原典型湖泊水文特征及关键影响因素

Hydrological Characteristics and Key Influencing Factors of Typical Lakes in the Qinghai Tibet Plateau from 1985 to 2021

张嘉琪 1张会兰 2刘雪妍1

作者信息

  • 1. 北京林业大学水土保持学院,北京 100083
  • 2. 北京林业大学水土保持学院,北京 100083||北京林业大学重庆缙云三峡库区森林生态系统国家定位观测研究站,重庆 400711
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摘要

Abstract

[Objective]The lakes of the Tibetan Plateau are important indicators of climate change,and their expansion or contraction also have an important impact on the natural environment of the Tibetan Plateau.[Methods]Three typical lakes located in different climatic sub-regions of the Qinghai-Tibet Plateau(Qinghai Lake,Yangzhuo Yongcuo,and Ulan Ula Lake)were selected to study the temporal and spatial variation of the hydrological characteristics of the three typical lakes from 1985 to 2021 by remote sensing monitoring methods,to reveal the role of key climatic factors,and to further explore the influence of glaciers and permafrost on the typical lakes.[Results]The area and water level of Qinghai Lake showed a significant upward trend,with an area increase of 238.68 km2 and a water level increase of 1.32 m.In space,it showed a trend of expansion in the east-west direction.The area and water level of Yangzhuo Yongcuo Lake first fluctuated and then decreased,decreasing by 16.31 km2 and 3.25 m respectively.In space,the overall area showed a shrinking trend from the surrounding to the center.The area and water level of Ulan Ula Lake showed a significant upward trend,increasing by 125.57 km2 and 8.12 m,respectively,and the expansion area was mainly concentrated in the south.[Conclusion]The analysis of key climate factors shows that the lake expansion caused by the increase of precipitation and the accelerated melting of glacial permafrost in the warm and humid environment is the most prominent environmental change characteristics of the Qinghai-Tibet Plateau.The main reason for the rise in the water level of Ulan Ula Lake is the seasonal thaw of permafrost caused by rising temperatures.Exploring the changes in lake area on the Tibetan Plateau is of great guiding significance for in-depth research on global climate change and surface water resource assessment.

关键词

青藏高原/湖泊/面积变化/水位/冰川冻土

Key words

Qinghai-Tibet Plateau/lakes/area change/water level/glacial permafrost

分类

天文与地球科学

引用本文复制引用

张嘉琪,张会兰,刘雪妍..1985-2021年青藏高原典型湖泊水文特征及关键影响因素[J].水土保持学报,2024,38(3):140-149,10.

基金项目

国家自然科学基金项目(52279056) (52279056)

水土保持学报

OA北大核心CSTPCD

1009-2242

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