Using Persistent Scatterer Interferometry to Map and Quantify Permafrost Thaw Subsidence: A Case Study of Eboling Mountain on the Qinghai-Tibet Plateau-Reference-Cited by-同舟云学术

Using Persistent Scatterer Interferometry to Map and Quantify Permafrost Thaw Subsidence: A Case Study of Eboling Mountain on the Qinghai-Tibet Plateau

Published:2018-10 Issue:10 Volume:123 Page:2663-2676
ISSN:2169-9003
Container-title:Journal of Geophysical Research: Earth Surface
language:en
Short-container-title:J. Geophys. Res. Earth Surf.

Author:

Chen Jie¹²³^ORCID,Liu Lin²^ORCID,Zhang Tingjun⁴^ORCID,Cao Bin⁴^ORCID,Lin Hui¹³⁵^ORCID

Affiliation:

1. Institute of Space and Earth Information Science; The Chinese University of Hong Kong; Hong Kong China

2. Earth System Science Programme, Faculty of Science; The Chinese University of Hong Kong; Hong Kong China

3. Shenzhen Research Institute; The Chinese University of Hong Kong; Shenzhen China

4. Key Laboratory of Western China's Environmental Systems; College of Earth and Environmental Sciences, Lanzhou University; Lanzhou China

5. Department of Geography and Resource Management; The Chinese University of Hong Kong; Hong Kong China

Funder

Chinese University of Hong Kong

Deutsches Zentrum für Luft- und Raumfahrt

Japan Aerospace Exploration Agency

Research Grants Council, University Grants Committee

Ministry of Science and Technology of the People's Republic of China

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2018JF004618/fullpdf

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5. Effects of thermo-erosional disturbance on surface soil carbon and nitrogen dynamics in upland arctic tundra;Camila;Environmental Research Letters,2014

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