Circumpolar mid-winter thaw and refreeze based on fusion of Metop ASCAT and SMOS, 2011/2012 - 2021/2022 ...
Rain-on-Snow (ROS) events occur across many regions of the terrestrial Arctic in mid-winter. Snow pack properties are changing and in extreme cases ice layers form which affect wildlife, vegetation and soils beyond the duration of the event. Active and passive microwave data have been combined to id...
Main Authors: | , , , , |
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Format: | Dataset |
Language: | English |
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Zenodo
2023
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Online Access: | https://dx.doi.org/10.5281/zenodo.7575926 https://zenodo.org/doi/10.5281/zenodo.7575926 |
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author | Bartsch, Annett Bergstedt, Helena Pointner, Georg Muri, Xaver Rautiainen, Kimmo |
author_facet | Bartsch, Annett Bergstedt, Helena Pointner, Georg Muri, Xaver Rautiainen, Kimmo |
author_sort | Bartsch, Annett |
collection | DataCite |
description | Rain-on-Snow (ROS) events occur across many regions of the terrestrial Arctic in mid-winter. Snow pack properties are changing and in extreme cases ice layers form which affect wildlife, vegetation and soils beyond the duration of the event. Active and passive microwave data have been combined to identify events over land North of 65°N (Bartsch et al. 2023). In a first step Metop ASCAT (C-Band radar) was used to identify potential sudden snow structure change. In a second step, results have been masked for coincident observation of wet snow within +- 3 days based on SMOS (derived from Centre Aval de Traitement des Données SMOS (CATDS) level 3 product). Note that the SMOS retrievals can have data gaps due to radio frequency interferences (RFI) what leads to gaps in the event detection. The dataset is structured by centre points of the hexagonal grid of the used Metop ASCAT product (EUMETSAT, approximately 12.5 km nominal resolution). Attributes include point ID (GPI), latitude, longitude and aggregated number ... : The study has received funding under the European Union's Horizon 2020 Research and Innovation Programme under Grant Agreement No. 869471 (CHARTER). This work was further supported by the European Space Agency CCI+ Permafrost project. ... |
format | Dataset |
genre | Arctic Ice permafrost |
genre_facet | Arctic Ice permafrost |
geographic | Arctic |
geographic_facet | Arctic |
id | ftdatacite:10.5281/zenodo.7575926 |
institution | Open Polar |
language | English |
op_collection_id | ftdatacite |
op_doi | https://doi.org/10.5281/zenodo.757592610.5194/tc-17-889-202310.5281/zenodo.7575927 |
op_relation | https://dx.doi.org/10.5194/tc-17-889-2023 https://dx.doi.org/10.5281/zenodo.7575927 |
op_rights | Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
publishDate | 2023 |
publisher | Zenodo |
record_format | openpolar |
spelling | ftdatacite:10.5281/zenodo.7575926 2025-01-16T20:29:02+00:00 Circumpolar mid-winter thaw and refreeze based on fusion of Metop ASCAT and SMOS, 2011/2012 - 2021/2022 ... Bartsch, Annett Bergstedt, Helena Pointner, Georg Muri, Xaver Rautiainen, Kimmo 2023 https://dx.doi.org/10.5281/zenodo.7575926 https://zenodo.org/doi/10.5281/zenodo.7575926 en eng Zenodo https://dx.doi.org/10.5194/tc-17-889-2023 https://dx.doi.org/10.5281/zenodo.7575927 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 rain-on-snow Arctic microwave remote sensing snow Dataset dataset 2023 ftdatacite https://doi.org/10.5281/zenodo.757592610.5194/tc-17-889-202310.5281/zenodo.7575927 2023-11-03T10:51:16Z Rain-on-Snow (ROS) events occur across many regions of the terrestrial Arctic in mid-winter. Snow pack properties are changing and in extreme cases ice layers form which affect wildlife, vegetation and soils beyond the duration of the event. Active and passive microwave data have been combined to identify events over land North of 65°N (Bartsch et al. 2023). In a first step Metop ASCAT (C-Band radar) was used to identify potential sudden snow structure change. In a second step, results have been masked for coincident observation of wet snow within +- 3 days based on SMOS (derived from Centre Aval de Traitement des Données SMOS (CATDS) level 3 product). Note that the SMOS retrievals can have data gaps due to radio frequency interferences (RFI) what leads to gaps in the event detection. The dataset is structured by centre points of the hexagonal grid of the used Metop ASCAT product (EUMETSAT, approximately 12.5 km nominal resolution). Attributes include point ID (GPI), latitude, longitude and aggregated number ... : The study has received funding under the European Union's Horizon 2020 Research and Innovation Programme under Grant Agreement No. 869471 (CHARTER). This work was further supported by the European Space Agency CCI+ Permafrost project. ... Dataset Arctic Ice permafrost DataCite Arctic |
spellingShingle | rain-on-snow Arctic microwave remote sensing snow Bartsch, Annett Bergstedt, Helena Pointner, Georg Muri, Xaver Rautiainen, Kimmo Circumpolar mid-winter thaw and refreeze based on fusion of Metop ASCAT and SMOS, 2011/2012 - 2021/2022 ... |
title | Circumpolar mid-winter thaw and refreeze based on fusion of Metop ASCAT and SMOS, 2011/2012 - 2021/2022 ... |
title_full | Circumpolar mid-winter thaw and refreeze based on fusion of Metop ASCAT and SMOS, 2011/2012 - 2021/2022 ... |
title_fullStr | Circumpolar mid-winter thaw and refreeze based on fusion of Metop ASCAT and SMOS, 2011/2012 - 2021/2022 ... |
title_full_unstemmed | Circumpolar mid-winter thaw and refreeze based on fusion of Metop ASCAT and SMOS, 2011/2012 - 2021/2022 ... |
title_short | Circumpolar mid-winter thaw and refreeze based on fusion of Metop ASCAT and SMOS, 2011/2012 - 2021/2022 ... |
title_sort | circumpolar mid-winter thaw and refreeze based on fusion of metop ascat and smos, 2011/2012 - 2021/2022 ... |
topic | rain-on-snow Arctic microwave remote sensing snow |
topic_facet | rain-on-snow Arctic microwave remote sensing snow |
url | https://dx.doi.org/10.5281/zenodo.7575926 https://zenodo.org/doi/10.5281/zenodo.7575926 |