PRODEM: Annual summer DEMs of the marginal areas of the Greenland Ice Sheet ...
Surface topography across the marginal zone of the Greenland Ice Sheet is constantly evolving in response to seasonal variability, longer-term climate change and glacier dynamics. Yet, current Digital Elevation Models (DEMs) for the ice sheet are usually based on data from a multi-year period, thus...
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2023
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Online Access: | https://dx.doi.org/10.22008/fk2/52wwhg https://dataverse.geus.dk/citation?persistentId=doi:10.22008/FK2/52WWHG |
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ftdatacite:10.22008/fk2/52wwhg 2024-09-30T14:35:22+00:00 PRODEM: Annual summer DEMs of the marginal areas of the Greenland Ice Sheet ... Winstrup, Mai 2023 https://dx.doi.org/10.22008/fk2/52wwhg https://dataverse.geus.dk/citation?persistentId=doi:10.22008/FK2/52WWHG unknown GEUS Dataverse https://dx.doi.org/10.22008/fk2/52wwhg/8jrbl5 https://dx.doi.org/10.22008/fk2/52wwhg/pew5f8 https://dx.doi.org/10.22008/fk2/52wwhg/opdoto https://dx.doi.org/10.22008/fk2/52wwhg/nonpcz https://dx.doi.org/10.22008/fk2/52wwhg/y0urhn https://dx.doi.org/10.22008/fk2/52wwhg/mgsioe https://dx.doi.org/10.22008/fk2/52wwhg/zmyygr https://dx.doi.org/10.22008/fk2/52wwhg/bfjeas https://dx.doi.org/10.22008/fk2/52wwhg/jabxsh https://dx.doi.org/10.22008/fk2/52wwhg/2x2ej1 https://dx.doi.org/10.22008/fk2/52wwhg/pxqgjw Dataset dataset 2023 ftdatacite https://doi.org/10.22008/fk2/52wwhg10.22008/fk2/52wwhg/8jrbl510.22008/fk2/52wwhg/pew5f810.22008/fk2/52wwhg/opdoto10.22008/fk2/52wwhg/nonpcz10.22008/fk2/52wwhg/y0urhn10.22008/fk2/52wwhg/mgsioe10.22008/fk2/52wwhg/zmyygr10.22008/fk2/52wwhg/bfjeas10.22008/fk2 2024-09-02T08:22:21Z Surface topography across the marginal zone of the Greenland Ice Sheet is constantly evolving in response to seasonal variability, longer-term climate change and glacier dynamics. Yet, current Digital Elevation Models (DEMs) for the ice sheet are usually based on data from a multi-year period, thus obscuring these changes over time. Here we present annual (2019-2022) summer DEMs in 500-meter resolution of the ice sheet marginal zone, a 50km wide band covering all outlet glaciers of the Greenland ice sheet. The annual summer DEMs follow the naming convention PRODEMxx, with xx being the year. ... Dataset glacier Greenland Ice Sheet DataCite Greenland |
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Open Polar |
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ftdatacite |
language |
unknown |
description |
Surface topography across the marginal zone of the Greenland Ice Sheet is constantly evolving in response to seasonal variability, longer-term climate change and glacier dynamics. Yet, current Digital Elevation Models (DEMs) for the ice sheet are usually based on data from a multi-year period, thus obscuring these changes over time. Here we present annual (2019-2022) summer DEMs in 500-meter resolution of the ice sheet marginal zone, a 50km wide band covering all outlet glaciers of the Greenland ice sheet. The annual summer DEMs follow the naming convention PRODEMxx, with xx being the year. ... |
format |
Dataset |
author |
Winstrup, Mai |
spellingShingle |
Winstrup, Mai PRODEM: Annual summer DEMs of the marginal areas of the Greenland Ice Sheet ... |
author_facet |
Winstrup, Mai |
author_sort |
Winstrup, Mai |
title |
PRODEM: Annual summer DEMs of the marginal areas of the Greenland Ice Sheet ... |
title_short |
PRODEM: Annual summer DEMs of the marginal areas of the Greenland Ice Sheet ... |
title_full |
PRODEM: Annual summer DEMs of the marginal areas of the Greenland Ice Sheet ... |
title_fullStr |
PRODEM: Annual summer DEMs of the marginal areas of the Greenland Ice Sheet ... |
title_full_unstemmed |
PRODEM: Annual summer DEMs of the marginal areas of the Greenland Ice Sheet ... |
title_sort |
prodem: annual summer dems of the marginal areas of the greenland ice sheet ... |
publisher |
GEUS Dataverse |
publishDate |
2023 |
url |
https://dx.doi.org/10.22008/fk2/52wwhg https://dataverse.geus.dk/citation?persistentId=doi:10.22008/FK2/52WWHG |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
glacier Greenland Ice Sheet |
genre_facet |
glacier Greenland Ice Sheet |
op_relation |
https://dx.doi.org/10.22008/fk2/52wwhg/8jrbl5 https://dx.doi.org/10.22008/fk2/52wwhg/pew5f8 https://dx.doi.org/10.22008/fk2/52wwhg/opdoto https://dx.doi.org/10.22008/fk2/52wwhg/nonpcz https://dx.doi.org/10.22008/fk2/52wwhg/y0urhn https://dx.doi.org/10.22008/fk2/52wwhg/mgsioe https://dx.doi.org/10.22008/fk2/52wwhg/zmyygr https://dx.doi.org/10.22008/fk2/52wwhg/bfjeas https://dx.doi.org/10.22008/fk2/52wwhg/jabxsh https://dx.doi.org/10.22008/fk2/52wwhg/2x2ej1 https://dx.doi.org/10.22008/fk2/52wwhg/pxqgjw |
op_doi |
https://doi.org/10.22008/fk2/52wwhg10.22008/fk2/52wwhg/8jrbl510.22008/fk2/52wwhg/pew5f810.22008/fk2/52wwhg/opdoto10.22008/fk2/52wwhg/nonpcz10.22008/fk2/52wwhg/y0urhn10.22008/fk2/52wwhg/mgsioe10.22008/fk2/52wwhg/zmyygr10.22008/fk2/52wwhg/bfjeas10.22008/fk2 |
_version_ |
1811638660336975872 |