3-D velocity field of the Tibetan Plateau due to land water loading

Table S1. 3-D velocity field of the Tibetan Plateau due to the loading of soil moisture. Table S2. 3-D velocity field of the Tibetan Plateau due to the loading of snow. Table S3. 3-D velocity field of the Tibetan Plateau due to the loading of glacier. Table S4. 3-D velocity field of the Tibetan Plat...

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Bibliographic Details
Main Author: Jiao, Jiashuang
Format: Other/Unknown Material
Language:English
Published: Jiashuang Jiao 2024
Subjects:
geodesy
Tibetan Plateau
crustal deformation
geophysics
mass transport
permafrost
Online Access:https://doi.org/10.5281/zenodo.11181483
Description
Summary:Table S1. 3-D velocity field of the Tibetan Plateau due to the loading of soil moisture. Table S2. 3-D velocity field of the Tibetan Plateau due to the loading of snow. Table S3. 3-D velocity field of the Tibetan Plateau due to the loading of glacier. Table S4. 3-D velocity field of the Tibetan Plateau due to the loading of lake. Table S5. 3-D velocity field of the Tibetan Plateau due to the loading of permafrost. Table S6. 3-D velocity field of the Tibetan Plateau due to the loading of groundwater.

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