Seasonal and Interannual Fluctuations of Glacier Mass Balance and Climate Response Processes on the Tibetan Plateau Based on GRACE/GRACE-FO
Author:
Affiliation:
1. Global Navigation Satellite System Research Center, Wuhan University, Wuhan, China
2. School of Geodesy and Geomatics, Wuhan University, Wuhan, China
3. School of Earth Science, The Ohio State University, Columbus, OH, USA
Funder
National Natural Science Foundation of China
Program for Hubei Provincial Science and Technology Innovation Talents
China Postdoctoral Science Foundation
Fundamental Research Funds for Central Universities
Open Research Fund Program of State Key Laboratory of Geodesy and Earth's Dynamics
Open Fund of Hubei Luojia Laboratory
Special Fund of Hubei Luojia Laboratory
Publisher
Institute of Electrical and Electronics Engineers (IEEE)
Subject
General Earth and Planetary Sciences,Electrical and Electronic Engineering
Link
http://xplorestaging.ieee.org/ielx7/36/10006360/10143379.pdf?arnumber=10143379
Reference52 articles.
1. Glacier mass changes on the Tibetan Plateau 2003–2009 derived from ICESat laser altimetry measurements
2. The European mountain cryosphere: a review of its current state, trends, and future challenges
3. High-frequency Holocene glacier fluctuations in the Himalayan-Tibetan orogen
4. Timing and climatic drivers for glaciation across semi-arid western Himalayan–Tibetan orogen
5. A Time‐Varying 3‐D Displacement Model of the ~5.9‐Year Westward Motion and its Applications for the Global Navigation Satellite System Positions and Velocities
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2. Glacier Mass Balance and Its Impact on Land Water Storage in the Southeastern Tibetan Plateau Revealed by ICESat-2 and GRACE-FO;Remote Sensing;2024-03-15
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