What Controls Lake Contraction and Then Expansion in Tibetan Plateau’s Endorheic Basin Over the Past Half Century?-Reference-Cited by-同舟云学术

What Controls Lake Contraction and Then Expansion in Tibetan Plateau’s Endorheic Basin Over the Past Half Century?

Published:2022-10-13 Issue:20 Volume:49 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Chen Wenfeng¹²,Liu Yong³,Zhang Guoqing¹^ORCID,Yang Kun⁴^ORCID,Zhou Tao¹²,Wang Jida⁵^ORCID,Shum C. K.⁶⁷^ORCID

Affiliation:

1. State Key Laboratory of Tibetan Plateau Earth System Resources and Environment (TPESER) Institute of Tibetan Plateau Research Chinese Academy of Sciences Beijing China

2. College of Resources and Environment University of Chinese Academy of Sciences Beijing China

3. Department of Atmospheric Science School of Environmental Studies China University of Geosciences Wuhan China

4. Ministry of Education Key Laboratory for Earth System Modelling Department of Earth System Science Tsinghua University Beijing China

5. Department of Geography and Geospatial Sciences Kansas State University Manhattan KS USA

6. Division of Geodetic Science School of Earth Sciences The Ohio State University Columbus OH USA

7. Innovation Academy for Precision Measurement Science and Technology Chinese Academy of Sciences Wuhan China

Funder

National Natural Science Foundation of China

Chinese Academy of Sciences

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GL101200

Reference46 articles.

1. Using GRACE to constrain precipitation amount over cold mountainous basins

2. Glacier topography and elevation changes derived from Pléiades sub-meter stereo images

3. High Mountain Asian glacier response to climate revealed by multi-temporal satellite observations since the 1960s

4. Differences in the water-balance components of four lakes in the southern-central Tibetan Plateau

5. A spatially resolved estimate of High Mountain Asia glacier mass balances from 2000 to 2016

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