The MOSAiC Drift: Ice conditions from space and comparison with previous years
We combine satellite data products to provide a first and general overview of the sea-ice conditions along the MOSAiC drift and a comparison with previous years. We find that the MOSAiC drift was around 25 % faster than the climatological mean drift, as a consequence of large-scale low-pressure anom...
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ftcopernicus:oai:publications.copernicus.org:tcd93296 2023-05-15T16:18:07+02:00 The MOSAiC Drift: Ice conditions from space and comparison with previous years Krumpen, Thomas Albedyll, Luisa Goessling, Helge F. Hendricks, Stefan Juhls, Bennet Spreen, Gunnar Willmes, Sascha Belter, H. Jakob Dethloff, Klaus Haas, Christian Kaleschke, Lars Katlein, Christian Tian-Kunze, Xiangshan Ricker, Robert Rostosky, Philip Rueckert, Janna Singha, Suman Sokolova, Julia 2021-04-08 application/pdf https://doi.org/10.5194/tc-2021-80 https://tc.copernicus.org/preprints/tc-2021-80/ eng eng doi:10.5194/tc-2021-80 https://tc.copernicus.org/preprints/tc-2021-80/ eISSN: 1994-0424 Text 2021 ftcopernicus https://doi.org/10.5194/tc-2021-80 2021-04-12T16:22:14Z We combine satellite data products to provide a first and general overview of the sea-ice conditions along the MOSAiC drift and a comparison with previous years. We find that the MOSAiC drift was around 25 % faster than the climatological mean drift, as a consequence of large-scale low-pressure anomalies prevailing around the Barents-Kara-Laptev Sea region between January and March. In winter (October–April), satellite observations show that the sea-ice in the vicinity of the Central Observatory (CO) was rather thin compared to the previous years along the same trajectory. Unlike ice thickness, satellite-derived sea-ice concentration, lead frequency, and snow thickness during winter month were close to the long-term mean with little variability. With the onset of spring and decreasing distance to Fram Strait, variability in ice concentration and lead activity increased. In addition, frequency and strength of deformation events (divergence and shear) were higher during summer than during winter. Overall, we find that sea-ice conditions observed close (~ 5 km) to the CO are representative for the wider (50 km and 100 km) surroundings. An exception is the ice thickness: Here we find that sea-ice near the CO (50 km radius) was 4 % thinner than sea-ice within a 100 km radius. Moreover, satellite acquisitions indicate that the formation of large melt ponds began earlier on the MOSAiC floe than on neighbouring floes. Text Fram Strait Kara-Laptev laptev Laptev Sea Sea ice Copernicus Publications: E-Journals Laptev Sea |
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Open Polar |
collection |
Copernicus Publications: E-Journals |
op_collection_id |
ftcopernicus |
language |
English |
description |
We combine satellite data products to provide a first and general overview of the sea-ice conditions along the MOSAiC drift and a comparison with previous years. We find that the MOSAiC drift was around 25 % faster than the climatological mean drift, as a consequence of large-scale low-pressure anomalies prevailing around the Barents-Kara-Laptev Sea region between January and March. In winter (October–April), satellite observations show that the sea-ice in the vicinity of the Central Observatory (CO) was rather thin compared to the previous years along the same trajectory. Unlike ice thickness, satellite-derived sea-ice concentration, lead frequency, and snow thickness during winter month were close to the long-term mean with little variability. With the onset of spring and decreasing distance to Fram Strait, variability in ice concentration and lead activity increased. In addition, frequency and strength of deformation events (divergence and shear) were higher during summer than during winter. Overall, we find that sea-ice conditions observed close (~ 5 km) to the CO are representative for the wider (50 km and 100 km) surroundings. An exception is the ice thickness: Here we find that sea-ice near the CO (50 km radius) was 4 % thinner than sea-ice within a 100 km radius. Moreover, satellite acquisitions indicate that the formation of large melt ponds began earlier on the MOSAiC floe than on neighbouring floes. |
format |
Text |
author |
Krumpen, Thomas Albedyll, Luisa Goessling, Helge F. Hendricks, Stefan Juhls, Bennet Spreen, Gunnar Willmes, Sascha Belter, H. Jakob Dethloff, Klaus Haas, Christian Kaleschke, Lars Katlein, Christian Tian-Kunze, Xiangshan Ricker, Robert Rostosky, Philip Rueckert, Janna Singha, Suman Sokolova, Julia |
spellingShingle |
Krumpen, Thomas Albedyll, Luisa Goessling, Helge F. Hendricks, Stefan Juhls, Bennet Spreen, Gunnar Willmes, Sascha Belter, H. Jakob Dethloff, Klaus Haas, Christian Kaleschke, Lars Katlein, Christian Tian-Kunze, Xiangshan Ricker, Robert Rostosky, Philip Rueckert, Janna Singha, Suman Sokolova, Julia The MOSAiC Drift: Ice conditions from space and comparison with previous years |
author_facet |
Krumpen, Thomas Albedyll, Luisa Goessling, Helge F. Hendricks, Stefan Juhls, Bennet Spreen, Gunnar Willmes, Sascha Belter, H. Jakob Dethloff, Klaus Haas, Christian Kaleschke, Lars Katlein, Christian Tian-Kunze, Xiangshan Ricker, Robert Rostosky, Philip Rueckert, Janna Singha, Suman Sokolova, Julia |
author_sort |
Krumpen, Thomas |
title |
The MOSAiC Drift: Ice conditions from space and comparison with previous years |
title_short |
The MOSAiC Drift: Ice conditions from space and comparison with previous years |
title_full |
The MOSAiC Drift: Ice conditions from space and comparison with previous years |
title_fullStr |
The MOSAiC Drift: Ice conditions from space and comparison with previous years |
title_full_unstemmed |
The MOSAiC Drift: Ice conditions from space and comparison with previous years |
title_sort |
mosaic drift: ice conditions from space and comparison with previous years |
publishDate |
2021 |
url |
https://doi.org/10.5194/tc-2021-80 https://tc.copernicus.org/preprints/tc-2021-80/ |
geographic |
Laptev Sea |
geographic_facet |
Laptev Sea |
genre |
Fram Strait Kara-Laptev laptev Laptev Sea Sea ice |
genre_facet |
Fram Strait Kara-Laptev laptev Laptev Sea Sea ice |
op_source |
eISSN: 1994-0424 |
op_relation |
doi:10.5194/tc-2021-80 https://tc.copernicus.org/preprints/tc-2021-80/ |
op_doi |
https://doi.org/10.5194/tc-2021-80 |
_version_ |
1766004242586271744 |