Vegetation green-up date is more sensitive to permafrost degradation than climate change in spring across the northern permafrost region
The material contains vegetation green-up date derived from GIMMS NDVI3g data (1982-2015), the start of thaw derived from FT-ESDR (1987-2017), and active layer thickness derived from daily mean temperature (1982-2017). The provided code is an example of conducting partial correlation analysis in thi...
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Online Access: | https://dx.doi.org/10.5281/zenodo.5728302 https://zenodo.org/record/5728302 |
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ftdatacite:10.5281/zenodo.5728302 2023-05-15T13:02:56+02:00 Vegetation green-up date is more sensitive to permafrost degradation than climate change in spring across the northern permafrost region Wang, Jian 2021 https://dx.doi.org/10.5281/zenodo.5728302 https://zenodo.org/record/5728302 unknown Zenodo https://dx.doi.org/10.5281/zenodo.5728303 Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess CC-BY article-journal ScholarlyArticle JournalArticle 2021 ftdatacite https://doi.org/10.5281/zenodo.5728302 https://doi.org/10.5281/zenodo.5728303 2022-02-08T14:57:16Z The material contains vegetation green-up date derived from GIMMS NDVI3g data (1982-2015), the start of thaw derived from FT-ESDR (1987-2017), and active layer thickness derived from daily mean temperature (1982-2017). The provided code is an example of conducting partial correlation analysis in this research. Article in Journal/Newspaper Active layer thickness permafrost DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
description |
The material contains vegetation green-up date derived from GIMMS NDVI3g data (1982-2015), the start of thaw derived from FT-ESDR (1987-2017), and active layer thickness derived from daily mean temperature (1982-2017). The provided code is an example of conducting partial correlation analysis in this research. |
format |
Article in Journal/Newspaper |
author |
Wang, Jian |
spellingShingle |
Wang, Jian Vegetation green-up date is more sensitive to permafrost degradation than climate change in spring across the northern permafrost region |
author_facet |
Wang, Jian |
author_sort |
Wang, Jian |
title |
Vegetation green-up date is more sensitive to permafrost degradation than climate change in spring across the northern permafrost region |
title_short |
Vegetation green-up date is more sensitive to permafrost degradation than climate change in spring across the northern permafrost region |
title_full |
Vegetation green-up date is more sensitive to permafrost degradation than climate change in spring across the northern permafrost region |
title_fullStr |
Vegetation green-up date is more sensitive to permafrost degradation than climate change in spring across the northern permafrost region |
title_full_unstemmed |
Vegetation green-up date is more sensitive to permafrost degradation than climate change in spring across the northern permafrost region |
title_sort |
vegetation green-up date is more sensitive to permafrost degradation than climate change in spring across the northern permafrost region |
publisher |
Zenodo |
publishDate |
2021 |
url |
https://dx.doi.org/10.5281/zenodo.5728302 https://zenodo.org/record/5728302 |
genre |
Active layer thickness permafrost |
genre_facet |
Active layer thickness permafrost |
op_relation |
https://dx.doi.org/10.5281/zenodo.5728303 |
op_rights |
Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5281/zenodo.5728302 https://doi.org/10.5281/zenodo.5728303 |
_version_ |
1766324440892702720 |