3-D velocity field of the Tibetan Plateau due to land water loading
Basicinformation: 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/10.10...
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Jiashuang Jiao
2024
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ftzenodo:oai:zenodo.org:12740076 2024-09-15T18:30:12+00:00 3-D velocity field of the Tibetan Plateau due to land water loading Jiao, Jiashuang 2024-07-14 https://doi.org/10.5281/zenodo.12740076 eng eng Jiashuang Jiao https://doi.org/10.5281/zenodo.10444131 https://doi.org/10.1029/2024GL108684 https://doi.org/10.5281/zenodo.10444130 https://doi.org/10.5281/zenodo.12740076 oai:zenodo.org:12740076 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode geodesy Tibetan Plateau crustal deformation geophysics mass transport GPS Earth and related environmental sciences info:eu-repo/semantics/other 2024 ftzenodo https://doi.org/10.5281/zenodo.1274007610.5281/zenodo.1044413110.1029/2024GL10868410.5281/zenodo.10444130 2024-07-26T15:47:26Z Basicinformation: 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 ... Other/Unknown Material permafrost ren Zenodo |
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English |
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geodesy Tibetan Plateau crustal deformation geophysics mass transport GPS Earth and related environmental sciences |
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geodesy Tibetan Plateau crustal deformation geophysics mass transport GPS Earth and related environmental sciences Jiao, Jiashuang 3-D velocity field of the Tibetan Plateau due to land water loading |
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geodesy Tibetan Plateau crustal deformation geophysics mass transport GPS Earth and related environmental sciences |
description |
Basicinformation: 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 ... |
format |
Other/Unknown Material |
author |
Jiao, Jiashuang |
author_facet |
Jiao, Jiashuang |
author_sort |
Jiao, Jiashuang |
title |
3-D velocity field of the Tibetan Plateau due to land water loading |
title_short |
3-D velocity field of the Tibetan Plateau due to land water loading |
title_full |
3-D velocity field of the Tibetan Plateau due to land water loading |
title_fullStr |
3-D velocity field of the Tibetan Plateau due to land water loading |
title_full_unstemmed |
3-D velocity field of the Tibetan Plateau due to land water loading |
title_sort |
3-d velocity field of the tibetan plateau due to land water loading |
publisher |
Jiashuang Jiao |
publishDate |
2024 |
url |
https://doi.org/10.5281/zenodo.12740076 |
genre |
permafrost ren |
genre_facet |
permafrost ren |
op_relation |
https://doi.org/10.5281/zenodo.10444131 https://doi.org/10.1029/2024GL108684 https://doi.org/10.5281/zenodo.10444130 https://doi.org/10.5281/zenodo.12740076 oai:zenodo.org:12740076 |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode |
op_doi |
https://doi.org/10.5281/zenodo.1274007610.5281/zenodo.1044413110.1029/2024GL10868410.5281/zenodo.10444130 |
_version_ |
1810471672160976896 |