DOI: 10.5281/zenodo.12740076
title: 3-D velocity field of the Tibetan Plateau due to land water loading

description: Basic information:

This dataset includes a series of 3-D loading deformation velocity fields, which are supplements to the GRL paper entitled "Present-Day Three-Dimensional Crustal Deformation Velocity of the Tibetan Plateau Due to Multi-Component Land Water Loading" [https://doi.org/10.1029/2024GL108684]. The deformation velocities are fitted using long time span data during 2000-2020, and the detailed description of the data processing and calculation methods can be found through the GRL paper. There are results of three different grid resolutions (0.5x0.5, 0.25x0.25, 0.1x0.1), and for distinction, different file naming suffixes are used. For example, '0point5grids' indicates the results are in 0.5-degree grid resolutions (0.5x0.5), and so forth.

Application scenario:

The velocity fields here can be directly used for the analysis of crustal deformation or used for the separation of land water-induced loading deformation within geodetic deformation velocity fields over Tibetan Plateau. There are results of all the six main land water components, including soil moisture (SM) [Table S1], snow water equivalent (SWE) [Table S2], glacier [Table S3], lake [Table S4], permafrost (PM) [Table S5] and groundwater storage (GWS) [Table S6], thus users can choose one or some they focus on, or directly choose the sum of all the six main components (i.e., GRACE-inferred total terrestrial water storage [Table S7]).

Citation: 

When using this dataset, please cite the GRL paper: Jiao, J., Pan, Y., Ren, D., & Zhang, X. (2024). Present-day three-dimensional crustal deformation velocity of the Tibetan Plateau due to multi-component land water loading. Geophysical Research Letters, 51, e2024GL108684. https://doi.org/10.1029/2024GL108684

Contents:

Table S1. 3-D velocity field of the Tibetan Plateau due to the loading of soil moisture (SM).

Table S2. 3-D velocity field of the Tibetan Plateau due to the loading of snow water equivalent (SWE).

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 (PM).

Table S6. 3-D velocity field of the Tibetan Plateau due to the loading of groundwater storage (GWS).Table S7. 3-D velocity field of the Tibetan Plateau due to the loading of GRACE-inferred total terrestrial water storage (TWS).
description: TableS1_0point5grids. 3-D velocity field of the Tibetan Plateau due to the loading of soil moisture (SM) [0.5-degree grid resolution].TableS1_0point25grids. 3-D velocity field of the Tibetan Plateau due to the loading of soil moisture (SM) [0.25-degree grid resolution].TableS1_0point1grids. 3-D velocity field of the Tibetan Plateau due to the loading of soil moisture (SM) [0.1-degree grid resolution].TableS2_0point5grids. 3-D velocity field of the Tibetan Plateau due to the loading of snow water equivalent (SWE) [0.5-degree grid resolution].TableS2_0point25grids. 3-D velocity field of the Tibetan Plateau due to the loading of snow water equivalent (SWE) [0.25-degree grid resolution].TableS2_0point1grids. 3-D velocity field of the Tibetan Plateau due to the loading of snow water equivalent (SWE) [0.1-degree grid resolution].TableS3_0point5grids. 3-D velocity field of the Tibetan Plateau due to the loading of glacier [0.5-degree grid resolution].TableS3_0point25grids. 3-D velocity field of the Tibetan Plateau due to the loading of glacier [0.25-degree grid resolution].TableS3_0point1grids. 3-D velocity field of the Tibetan Plateau due to the loading of glacier [0.1-degree grid resolution].TableS4_0point5grids. 3-D velocity field of the Tibetan Plateau due to the loading of lake [0.5-degree grid resolution].TableS4_0point25grids. 3-D velocity field of the Tibetan Plateau due to the loading of lake [0.25-degree grid resolution].TableS4_0point1grids. 3-D velocity field of the Tibetan Plateau due to the loading of lake [0.1-degree grid resolution].TableS5_0point5grids. 3-D velocity field of the Tibetan Plateau due to the loading of permafrost (PM) [0.5-degree grid resolution].TableS5_0point25grids. 3-D velocity field of the Tibetan Plateau due to the loading of permafrost (PM) [0.25-degree grid resolution].TableS5_0point1grids. 3-D velocity field of the Tibetan Plateau due to the loading of permafrost (PM) [0.1-degree grid resolution].TableS6_0point5grids. 3-D velocity field of the Tibetan Plateau due to the loading of groundwater storage (GWS) [0.5-degree grid resolution].TableS6_0point25grids. 3-D velocity field of the Tibetan Plateau due to the loading of groundwater storage (GWS) [0.25-degree grid resolution].TableS6_0point1grids. 3-D velocity field of the Tibetan Plateau due to the loading of groundwater storage (GWS) [0.1-degree grid resolution].TableS7_0point5grids. 3-D velocity field of the Tibetan Plateau due to the loading of GRACE-inferred total terrestrial water storage (TWS) [0.5-degree grid resolution].TableS7_0point25grids. 3-D velocity field of the Tibetan Plateau due to the loading of GRACE-inferred total terrestrial water storage (TWS) [0.25-degree grid resolution].TableS7_0point1grids. 3-D velocity field of the Tibetan Plateau due to the loading of GRACE-inferred total terrestrial water storage (TWS) [0.1-degree grid resolution].