SIMBA data acquired during IAOOS drifts from the North-Pole to Fram Strait in 2013 ...
We report continuous observations in the high Arctic (north of 84°N) over the full 2013 summer season at two nearby sites with distinct initial snow depth, ice thickness and altitude with respect to the local ice topography. The two sites subject to similar atmospheric conditions that did not favor...
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Online Access: | https://dx.doi.org/10.17882/58796 https://www.seanoe.org/data/00476/58796/ |
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ftdatacite:10.17882/58796 2023-11-05T03:39:44+01:00 SIMBA data acquired during IAOOS drifts from the North-Pole to Fram Strait in 2013 ... Sennechael, Nathalie Provost, Christine Gascard, Jean-Claude Calzas, Michel Drezen, Christine Garracio, Magali 2019 https://dx.doi.org/10.17882/58796 https://www.seanoe.org/data/00476/58796/ unknown SEANOE CC-BY-NC https://creativecommons.org/licenses/by-nc/4.0 sea ice snow melt melt pond false bottom mass balance ice topography Dataset dataset 2019 ftdatacite https://doi.org/10.17882/58796 2023-10-09T10:18:59Z We report continuous observations in the high Arctic (north of 84°N) over the full 2013 summer season at two nearby sites with distinct initial snow depth, ice thickness and altitude with respect to the local ice topography. The two sites subject to similar atmospheric conditions that did not favor strong ice melt showed a contrasted evolution. One site, with an initial thin sea ice (1.40 m) at a low location of the floe, witnessed the formation of a spectacular 1.20 m-deep melt pond, a pond-enhanced erosion of the ice surface and a sudden pond drainage into the ocean. Then, the outpoured fresh water rapidly froze, heated the old ice from below and also acted as a temporary shield from the ocean heat flux while it was progressively ablated through dissolution. Eventually, the site almost recovered its initial ice thickness. In contrast, the other site, with an initial thicker sea ice (1.75 m) at a high location of the floe, did not support any significant melt water and underwent over 0.5 m of continuous ... Dataset Arctic Fram Strait North Pole Sea ice DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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unknown |
topic |
sea ice snow melt melt pond false bottom mass balance ice topography |
spellingShingle |
sea ice snow melt melt pond false bottom mass balance ice topography Sennechael, Nathalie Provost, Christine Gascard, Jean-Claude Calzas, Michel Drezen, Christine Garracio, Magali SIMBA data acquired during IAOOS drifts from the North-Pole to Fram Strait in 2013 ... |
topic_facet |
sea ice snow melt melt pond false bottom mass balance ice topography |
description |
We report continuous observations in the high Arctic (north of 84°N) over the full 2013 summer season at two nearby sites with distinct initial snow depth, ice thickness and altitude with respect to the local ice topography. The two sites subject to similar atmospheric conditions that did not favor strong ice melt showed a contrasted evolution. One site, with an initial thin sea ice (1.40 m) at a low location of the floe, witnessed the formation of a spectacular 1.20 m-deep melt pond, a pond-enhanced erosion of the ice surface and a sudden pond drainage into the ocean. Then, the outpoured fresh water rapidly froze, heated the old ice from below and also acted as a temporary shield from the ocean heat flux while it was progressively ablated through dissolution. Eventually, the site almost recovered its initial ice thickness. In contrast, the other site, with an initial thicker sea ice (1.75 m) at a high location of the floe, did not support any significant melt water and underwent over 0.5 m of continuous ... |
format |
Dataset |
author |
Sennechael, Nathalie Provost, Christine Gascard, Jean-Claude Calzas, Michel Drezen, Christine Garracio, Magali |
author_facet |
Sennechael, Nathalie Provost, Christine Gascard, Jean-Claude Calzas, Michel Drezen, Christine Garracio, Magali |
author_sort |
Sennechael, Nathalie |
title |
SIMBA data acquired during IAOOS drifts from the North-Pole to Fram Strait in 2013 ... |
title_short |
SIMBA data acquired during IAOOS drifts from the North-Pole to Fram Strait in 2013 ... |
title_full |
SIMBA data acquired during IAOOS drifts from the North-Pole to Fram Strait in 2013 ... |
title_fullStr |
SIMBA data acquired during IAOOS drifts from the North-Pole to Fram Strait in 2013 ... |
title_full_unstemmed |
SIMBA data acquired during IAOOS drifts from the North-Pole to Fram Strait in 2013 ... |
title_sort |
simba data acquired during iaoos drifts from the north-pole to fram strait in 2013 ... |
publisher |
SEANOE |
publishDate |
2019 |
url |
https://dx.doi.org/10.17882/58796 https://www.seanoe.org/data/00476/58796/ |
genre |
Arctic Fram Strait North Pole Sea ice |
genre_facet |
Arctic Fram Strait North Pole Sea ice |
op_rights |
CC-BY-NC https://creativecommons.org/licenses/by-nc/4.0 |
op_doi |
https://doi.org/10.17882/58796 |
_version_ |
1781695635603324928 |