The Antarctic sea ice cover from ICESat-2 and CryoSat-2: freeboard, snow depth and ice thickness
We offer a view of the Antarctic sea ice cover from lidar (ICESat-2) and radar (CryoSat-2) altimetry, with retrievals of freeboards, snow depth, and ice volume that span an 8-month winter between April 2019 and November 2019. Snow depths are from freeboard differences. The multiyear ice in the West...
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ftcopernicus:oai:publications.copernicus.org:tcd85970 2023-05-15T13:24:13+02:00 The Antarctic sea ice cover from ICESat-2 and CryoSat-2: freeboard, snow depth and ice thickness Kacimi, Sahra Kwok, Ron 2020-06-12 application/pdf https://doi.org/10.5194/tc-2020-145 https://tc.copernicus.org/preprints/tc-2020-145/ eng eng doi:10.5194/tc-2020-145 https://tc.copernicus.org/preprints/tc-2020-145/ eISSN: 1994-0424 Text 2020 ftcopernicus https://doi.org/10.5194/tc-2020-145 2020-07-20T16:22:06Z We offer a view of the Antarctic sea ice cover from lidar (ICESat-2) and radar (CryoSat-2) altimetry, with retrievals of freeboards, snow depth, and ice volume that span an 8-month winter between April 2019 and November 2019. Snow depths are from freeboard differences. The multiyear ice in the West Weddell sector stands out with a mean sector thickness > 2 m. Thinnest ice is found near polynyas (Ross Sea and Ronne) where new ice areas are exported seaward and entrained in the surrounding ice cover. For all months, the results suggest that ~ 60–70 % of the total freeboard is comprised of snow. The remarkable response of the ice cover to mechanical convergence in the coastal Amundsen Sea, associated with onshore winds, was captured in the correlated increase in local freeboards and thickness. While the spatial patterns in the freeboard, snow depth, and thickness composites are as expected, the observed seasonality in these variables is surprisingly weak likely attributable to competing processes (snowfall, snow redistribution, snow-ice formation, ice deformation, basal growth/melt) that contribute to uncorrelated changes in the total and radar freeboards. Broadly, evidence points to biases in CryoSat-2 freeboards of at least a few centimeters from high salinity snow (> 10 psu) in the basal layer resulting in lower/higher snow depth/ice thickness retrievals although the extent of these areas cannot be established in the current data set. Adjusting CryoSat-2 freeboards by 3/6 cm gives a circumpolar ice volume of 14,700/12,400 km 3 in October, for an average thickness of ~ 1.09/0.93 m. Validation of Antarctic sea ice parameters remains a challenge, there are no seasonally and regionally diverse data sets that could be used to assess these large-scale satellite retrievals. Text Amundsen Sea Antarc* Antarctic Ross Sea Sea ice Copernicus Publications: E-Journals Amundsen Sea Antarctic Ross Sea The Antarctic Weddell |
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Open Polar |
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Copernicus Publications: E-Journals |
op_collection_id |
ftcopernicus |
language |
English |
description |
We offer a view of the Antarctic sea ice cover from lidar (ICESat-2) and radar (CryoSat-2) altimetry, with retrievals of freeboards, snow depth, and ice volume that span an 8-month winter between April 2019 and November 2019. Snow depths are from freeboard differences. The multiyear ice in the West Weddell sector stands out with a mean sector thickness > 2 m. Thinnest ice is found near polynyas (Ross Sea and Ronne) where new ice areas are exported seaward and entrained in the surrounding ice cover. For all months, the results suggest that ~ 60–70 % of the total freeboard is comprised of snow. The remarkable response of the ice cover to mechanical convergence in the coastal Amundsen Sea, associated with onshore winds, was captured in the correlated increase in local freeboards and thickness. While the spatial patterns in the freeboard, snow depth, and thickness composites are as expected, the observed seasonality in these variables is surprisingly weak likely attributable to competing processes (snowfall, snow redistribution, snow-ice formation, ice deformation, basal growth/melt) that contribute to uncorrelated changes in the total and radar freeboards. Broadly, evidence points to biases in CryoSat-2 freeboards of at least a few centimeters from high salinity snow (> 10 psu) in the basal layer resulting in lower/higher snow depth/ice thickness retrievals although the extent of these areas cannot be established in the current data set. Adjusting CryoSat-2 freeboards by 3/6 cm gives a circumpolar ice volume of 14,700/12,400 km 3 in October, for an average thickness of ~ 1.09/0.93 m. Validation of Antarctic sea ice parameters remains a challenge, there are no seasonally and regionally diverse data sets that could be used to assess these large-scale satellite retrievals. |
format |
Text |
author |
Kacimi, Sahra Kwok, Ron |
spellingShingle |
Kacimi, Sahra Kwok, Ron The Antarctic sea ice cover from ICESat-2 and CryoSat-2: freeboard, snow depth and ice thickness |
author_facet |
Kacimi, Sahra Kwok, Ron |
author_sort |
Kacimi, Sahra |
title |
The Antarctic sea ice cover from ICESat-2 and CryoSat-2: freeboard, snow depth and ice thickness |
title_short |
The Antarctic sea ice cover from ICESat-2 and CryoSat-2: freeboard, snow depth and ice thickness |
title_full |
The Antarctic sea ice cover from ICESat-2 and CryoSat-2: freeboard, snow depth and ice thickness |
title_fullStr |
The Antarctic sea ice cover from ICESat-2 and CryoSat-2: freeboard, snow depth and ice thickness |
title_full_unstemmed |
The Antarctic sea ice cover from ICESat-2 and CryoSat-2: freeboard, snow depth and ice thickness |
title_sort |
antarctic sea ice cover from icesat-2 and cryosat-2: freeboard, snow depth and ice thickness |
publishDate |
2020 |
url |
https://doi.org/10.5194/tc-2020-145 https://tc.copernicus.org/preprints/tc-2020-145/ |
geographic |
Amundsen Sea Antarctic Ross Sea The Antarctic Weddell |
geographic_facet |
Amundsen Sea Antarctic Ross Sea The Antarctic Weddell |
genre |
Amundsen Sea Antarc* Antarctic Ross Sea Sea ice |
genre_facet |
Amundsen Sea Antarc* Antarctic Ross Sea Sea ice |
op_source |
eISSN: 1994-0424 |
op_relation |
doi:10.5194/tc-2020-145 https://tc.copernicus.org/preprints/tc-2020-145/ |
op_doi |
https://doi.org/10.5194/tc-2020-145 |
_version_ |
1766378138067009536 |