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 13:00:00UTC to July 9, 2018 at 22:00:00UTC represented as the logarithm of the signal...
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ftzenodo:oai:zenodo.org:5602842 2024-09-15T18:09:32+00:00 Animation of consecutive TRI intensity images at the front of Eqip Sermia, Greenland Adrien Wehrlé 2021-10-27 https://doi.org/10.5281/zenodo.5602842 unknown Zenodo https://doi.org/10.5281/zenodo.5602841 https://doi.org/10.5281/zenodo.5602842 oai:zenodo.org:5602842 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode info:eu-repo/semantics/other 2021 ftzenodo https://doi.org/10.5281/zenodo.560284210.5281/zenodo.5602841 2024-07-27T04:18:37Z 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 13:00:00UTC to July 9, 2018 at 22:00:00UTC 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. Other/Unknown Material Greenland Zenodo |
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Open Polar |
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ftzenodo |
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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 13:00:00UTC to July 9, 2018 at 22:00:00UTC 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 |
Other/Unknown Material |
author |
Adrien Wehrlé |
spellingShingle |
Adrien Wehrlé Animation of consecutive TRI intensity images at the front of Eqip Sermia, Greenland |
author_facet |
Adrien Wehrlé |
author_sort |
Adrien Wehrlé |
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://doi.org/10.5281/zenodo.5602842 |
genre |
Greenland |
genre_facet |
Greenland |
op_relation |
https://doi.org/10.5281/zenodo.5602841 https://doi.org/10.5281/zenodo.5602842 oai:zenodo.org:5602842 |
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.560284210.5281/zenodo.5602841 |
_version_ |
1810447100477964288 |