Animation of consecutive TRI intensity images at the front of Eqip Sermia, Greenland
Appendix C1 of a prepint published in The Cryosphere Discussions (at the release date): https://tc.copernicus.org/preprints/tc-2021-33/ Animation of consecutive one-minute interval radar images from July 9, 2018 at 13:00:00 UTC to July 9, 2018 at 22:00:00 UTC represented as the logarithm of the sign...
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ftdatacite:10.5281/zenodo.5602842 2023-05-15T16:28:24+02:00 Animation of consecutive TRI intensity images at the front of Eqip Sermia, Greenland Wehrlé, Adrien 2021 https://dx.doi.org/10.5281/zenodo.5602842 https://zenodo.org/record/5602842 unknown Zenodo https://dx.doi.org/10.5281/zenodo.5602841 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 MediaObject Audiovisual 2021 ftdatacite https://doi.org/10.5281/zenodo.5602842 https://doi.org/10.5281/zenodo.5602841 2022-02-08T12:05:56Z Appendix C1 of a prepint published in The Cryosphere Discussions (at the release date): https://tc.copernicus.org/preprints/tc-2021-33/ Animation of consecutive one-minute interval radar images from July 9, 2018 at 13:00:00 UTC to July 9, 2018 at 22:00:00 UTC represented as the logarithm of the signal strength. Clearly visible is the evolution of a meltwater plume footprint in the deep sector, pushing the ice debris coverage away from the calving front therefore creating an open water area. Short-lived wave trains generated by falling ice chunks along the calving front are also discernible as they propagate through the ocean ice cover. Article in Journal/Newspaper Greenland DataCite Metadata Store (German National Library of Science and Technology) Greenland Eqip Sermia ENVELOPE(-50.067,-50.067,69.817,69.817) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
description |
Appendix C1 of a prepint published in The Cryosphere Discussions (at the release date): https://tc.copernicus.org/preprints/tc-2021-33/ Animation of consecutive one-minute interval radar images from July 9, 2018 at 13:00:00 UTC to July 9, 2018 at 22:00:00 UTC represented as the logarithm of the signal strength. Clearly visible is the evolution of a meltwater plume footprint in the deep sector, pushing the ice debris coverage away from the calving front therefore creating an open water area. Short-lived wave trains generated by falling ice chunks along the calving front are also discernible as they propagate through the ocean ice cover. |
format |
Article in Journal/Newspaper |
author |
Wehrlé, Adrien |
spellingShingle |
Wehrlé, Adrien Animation of consecutive TRI intensity images at the front of Eqip Sermia, Greenland |
author_facet |
Wehrlé, Adrien |
author_sort |
Wehrlé, Adrien |
title |
Animation of consecutive TRI intensity images at the front of Eqip Sermia, Greenland |
title_short |
Animation of consecutive TRI intensity images at the front of Eqip Sermia, Greenland |
title_full |
Animation of consecutive TRI intensity images at the front of Eqip Sermia, Greenland |
title_fullStr |
Animation of consecutive TRI intensity images at the front of Eqip Sermia, Greenland |
title_full_unstemmed |
Animation of consecutive TRI intensity images at the front of Eqip Sermia, Greenland |
title_sort |
animation of consecutive tri intensity images at the front of eqip sermia, greenland |
publisher |
Zenodo |
publishDate |
2021 |
url |
https://dx.doi.org/10.5281/zenodo.5602842 https://zenodo.org/record/5602842 |
long_lat |
ENVELOPE(-50.067,-50.067,69.817,69.817) |
geographic |
Greenland Eqip Sermia |
geographic_facet |
Greenland Eqip Sermia |
genre |
Greenland |
genre_facet |
Greenland |
op_relation |
https://dx.doi.org/10.5281/zenodo.5602841 |
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.5602842 https://doi.org/10.5281/zenodo.5602841 |
_version_ |
1766018051642228736 |