IAOOS winter SIMBA data during N-ICE 2015 North of Svalbard ...

Two ice mass balance instruments (part of IAOOS7 and IAOOS8 platforms) deployed near 83°N on the same ice floe, documented the evolution of snow and ice conditions in the Arctic Ocean north of Svalbard in Jan-Mar 2015. Frequent profiles of temperature (every 3 hours) and temperature change after 30s...

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Bibliographic Details
Main Authors: Sennéchael, Nathalie, Provost, Christine, Villacieros-Robineau, Nicolas, Calzas, Michel, Guillot, Antoine, Savy, Jean-Philippe, Garracio, Magali, Koenig, Zoé
Format: Dataset
Language:unknown
Published: SEANOE 2015
Subjects:
Online Access:https://dx.doi.org/10.17882/59624
https://www.seanoe.org/data/00485/59624/
id ftdatacite:10.17882/59624
record_format openpolar
spelling ftdatacite:10.17882/59624 2023-11-05T03:39:41+01:00 IAOOS winter SIMBA data during N-ICE 2015 North of Svalbard ... Sennéchael, Nathalie Provost, Christine Villacieros-Robineau, Nicolas Calzas, Michel Guillot, Antoine Savy, Jean-Philippe Garracio, Magali Koenig, Zoé 2015 https://dx.doi.org/10.17882/59624 https://www.seanoe.org/data/00485/59624/ unknown SEANOE https://dx.doi.org/10.17882/59516 https://dx.doi.org/10.1002/2017jc013328 https://dx.doi.org/10.1002/2016jc012011 https://dx.doi.org/10.1002/2016jc012195 https://dx.doi.org/10.1175/jtech-d-13-00058.1 CC-BY-NC https://creativecommons.org/licenses/by-nc/4.0 sea ice snow ice growth basal melt flooding snow-ice mass balance Dataset dataset 2015 ftdatacite https://doi.org/10.17882/5962410.17882/5951610.1002/2017jc01332810.1002/2016jc01201110.1002/2016jc01219510.1175/jtech-d-13-00058.1 2023-10-09T10:49:06Z Two ice mass balance instruments (part of IAOOS7 and IAOOS8 platforms) deployed near 83°N on the same ice floe, documented the evolution of snow and ice conditions in the Arctic Ocean north of Svalbard in Jan-Mar 2015. Frequent profiles of temperature (every 3 hours) and temperature change after 30s and 120s heating (once a day) were recorded. The ratio of the temperature changes after heating provides a proxy for thermal diffusivity. Both instruments documented flooding and snow-ice formation. Flooding was clearly detectable in the simultaneous changes in thermal diffusivity proxy, increased temperature, and heat propagation through the underlying ice. Slush then progressively transformed into snow-ice. Flooding resulted from two different processes; i) after storm-induced break-up of snow-loaded floes for IAOOS8 and ii) after loss of buoyancy due to basal ice melt for IAOOS7. The instrument on IAOOS7 documented basal sea-ice melt over warm Atlantic waters and ocean-to-ice heat flux peaked at up to 400 Wm-2 ... Dataset Arctic Arctic Ocean Sea ice Svalbard 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
topic sea ice
snow
ice growth
basal melt
flooding
snow-ice
mass balance
spellingShingle sea ice
snow
ice growth
basal melt
flooding
snow-ice
mass balance
Sennéchael, Nathalie
Provost, Christine
Villacieros-Robineau, Nicolas
Calzas, Michel
Guillot, Antoine
Savy, Jean-Philippe
Garracio, Magali
Koenig, Zoé
IAOOS winter SIMBA data during N-ICE 2015 North of Svalbard ...
topic_facet sea ice
snow
ice growth
basal melt
flooding
snow-ice
mass balance
description Two ice mass balance instruments (part of IAOOS7 and IAOOS8 platforms) deployed near 83°N on the same ice floe, documented the evolution of snow and ice conditions in the Arctic Ocean north of Svalbard in Jan-Mar 2015. Frequent profiles of temperature (every 3 hours) and temperature change after 30s and 120s heating (once a day) were recorded. The ratio of the temperature changes after heating provides a proxy for thermal diffusivity. Both instruments documented flooding and snow-ice formation. Flooding was clearly detectable in the simultaneous changes in thermal diffusivity proxy, increased temperature, and heat propagation through the underlying ice. Slush then progressively transformed into snow-ice. Flooding resulted from two different processes; i) after storm-induced break-up of snow-loaded floes for IAOOS8 and ii) after loss of buoyancy due to basal ice melt for IAOOS7. The instrument on IAOOS7 documented basal sea-ice melt over warm Atlantic waters and ocean-to-ice heat flux peaked at up to 400 Wm-2 ...
format Dataset
author Sennéchael, Nathalie
Provost, Christine
Villacieros-Robineau, Nicolas
Calzas, Michel
Guillot, Antoine
Savy, Jean-Philippe
Garracio, Magali
Koenig, Zoé
author_facet Sennéchael, Nathalie
Provost, Christine
Villacieros-Robineau, Nicolas
Calzas, Michel
Guillot, Antoine
Savy, Jean-Philippe
Garracio, Magali
Koenig, Zoé
author_sort Sennéchael, Nathalie
title IAOOS winter SIMBA data during N-ICE 2015 North of Svalbard ...
title_short IAOOS winter SIMBA data during N-ICE 2015 North of Svalbard ...
title_full IAOOS winter SIMBA data during N-ICE 2015 North of Svalbard ...
title_fullStr IAOOS winter SIMBA data during N-ICE 2015 North of Svalbard ...
title_full_unstemmed IAOOS winter SIMBA data during N-ICE 2015 North of Svalbard ...
title_sort iaoos winter simba data during n-ice 2015 north of svalbard ...
publisher SEANOE
publishDate 2015
url https://dx.doi.org/10.17882/59624
https://www.seanoe.org/data/00485/59624/
genre Arctic
Arctic Ocean
Sea ice
Svalbard
genre_facet Arctic
Arctic Ocean
Sea ice
Svalbard
op_relation https://dx.doi.org/10.17882/59516
https://dx.doi.org/10.1002/2017jc013328
https://dx.doi.org/10.1002/2016jc012011
https://dx.doi.org/10.1002/2016jc012195
https://dx.doi.org/10.1175/jtech-d-13-00058.1
op_rights CC-BY-NC
https://creativecommons.org/licenses/by-nc/4.0
op_doi https://doi.org/10.17882/5962410.17882/5951610.1002/2017jc01332810.1002/2016jc01201110.1002/2016jc01219510.1175/jtech-d-13-00058.1
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