IWWOC Antarctic Sea Ice Backscatter Gridded Level 3 Composite from SCAT onboard CFOSAT ...
Backscatter values over sea ice are a function of incidence angle and the sea ice type. With several SCAT incidence measurements, an incidence adjustment is mandatory over sea ice (Gohin and Cavanié 1994) to map daily averaged backscatter values accurately for geophysical use as it was done for the...
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Ifremer / CERSAT
2022
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Online Access: | https://dx.doi.org/10.12770/1241fd87-dfc6-4be1-9bfe-7bc222f9d785 https://sextant.ifremer.fr/record/1241fd87-dfc6-4be1-9bfe-7bc222f9d785 |
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ftdatacite:10.12770/1241fd87-dfc6-4be1-9bfe-7bc222f9d785 2023-10-01T03:51:59+02:00 IWWOC Antarctic Sea Ice Backscatter Gridded Level 3 Composite from SCAT onboard CFOSAT ... Ardhuin, Fanny 2022 https://dx.doi.org/10.12770/1241fd87-dfc6-4be1-9bfe-7bc222f9d785 https://sextant.ifremer.fr/record/1241fd87-dfc6-4be1-9bfe-7bc222f9d785 unknown Ifremer / CERSAT Oceanographic geographical features Sea Ice CFOSAT Less than 4 days /Sea Ice/Ice Roughness /Sea Ice/Ice Extent CDS-SAT-CERSAT /Physical Oceanography/Sea Ice /Remote sensing Remote sensing Dataset dataset series/Series 2022 ftdatacite https://doi.org/10.12770/1241fd87-dfc6-4be1-9bfe-7bc222f9d785 2023-09-04T13:08:17Z Backscatter values over sea ice are a function of incidence angle and the sea ice type. With several SCAT incidence measurements, an incidence adjustment is mandatory over sea ice (Gohin and Cavanié 1994) to map daily averaged backscatter values accurately for geophysical use as it was done for the NSCAT Ku-band sensor. An incidence-adjustment backscatter map at 40° incidence angle is thus built in order to have reliable daily averaged backscatter maps. This dataset contains antarctic polar stereographic 12 km resolution grids of averaged backscatter coefficient from SCAT onboard CFOSAT scatterometer over sea-ice, for each polarization (HH and VV). CFOSAT (Chinese French Ocean SATellite) is a french-chinese mission launched in 2018, whose aim is to provide wind (SCAT instrument) and wave (SWIM instrument) measurements over the sea surface. The grids are derived from swath sigma-naught data (CWWIC SCAT Level 1A product), averaged over one day. Sea ice roughness from the scatterometer backscatter can be used ... Dataset Antarc* Antarctic Sea ice DataCite Metadata Store (German National Library of Science and Technology) Antarctic |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Oceanographic geographical features Sea Ice CFOSAT Less than 4 days /Sea Ice/Ice Roughness /Sea Ice/Ice Extent CDS-SAT-CERSAT /Physical Oceanography/Sea Ice /Remote sensing Remote sensing |
spellingShingle |
Oceanographic geographical features Sea Ice CFOSAT Less than 4 days /Sea Ice/Ice Roughness /Sea Ice/Ice Extent CDS-SAT-CERSAT /Physical Oceanography/Sea Ice /Remote sensing Remote sensing Ardhuin, Fanny IWWOC Antarctic Sea Ice Backscatter Gridded Level 3 Composite from SCAT onboard CFOSAT ... |
topic_facet |
Oceanographic geographical features Sea Ice CFOSAT Less than 4 days /Sea Ice/Ice Roughness /Sea Ice/Ice Extent CDS-SAT-CERSAT /Physical Oceanography/Sea Ice /Remote sensing Remote sensing |
description |
Backscatter values over sea ice are a function of incidence angle and the sea ice type. With several SCAT incidence measurements, an incidence adjustment is mandatory over sea ice (Gohin and Cavanié 1994) to map daily averaged backscatter values accurately for geophysical use as it was done for the NSCAT Ku-band sensor. An incidence-adjustment backscatter map at 40° incidence angle is thus built in order to have reliable daily averaged backscatter maps. This dataset contains antarctic polar stereographic 12 km resolution grids of averaged backscatter coefficient from SCAT onboard CFOSAT scatterometer over sea-ice, for each polarization (HH and VV). CFOSAT (Chinese French Ocean SATellite) is a french-chinese mission launched in 2018, whose aim is to provide wind (SCAT instrument) and wave (SWIM instrument) measurements over the sea surface. The grids are derived from swath sigma-naught data (CWWIC SCAT Level 1A product), averaged over one day. Sea ice roughness from the scatterometer backscatter can be used ... |
format |
Dataset |
author |
Ardhuin, Fanny |
author_facet |
Ardhuin, Fanny |
author_sort |
Ardhuin, Fanny |
title |
IWWOC Antarctic Sea Ice Backscatter Gridded Level 3 Composite from SCAT onboard CFOSAT ... |
title_short |
IWWOC Antarctic Sea Ice Backscatter Gridded Level 3 Composite from SCAT onboard CFOSAT ... |
title_full |
IWWOC Antarctic Sea Ice Backscatter Gridded Level 3 Composite from SCAT onboard CFOSAT ... |
title_fullStr |
IWWOC Antarctic Sea Ice Backscatter Gridded Level 3 Composite from SCAT onboard CFOSAT ... |
title_full_unstemmed |
IWWOC Antarctic Sea Ice Backscatter Gridded Level 3 Composite from SCAT onboard CFOSAT ... |
title_sort |
iwwoc antarctic sea ice backscatter gridded level 3 composite from scat onboard cfosat ... |
publisher |
Ifremer / CERSAT |
publishDate |
2022 |
url |
https://dx.doi.org/10.12770/1241fd87-dfc6-4be1-9bfe-7bc222f9d785 https://sextant.ifremer.fr/record/1241fd87-dfc6-4be1-9bfe-7bc222f9d785 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Sea ice |
genre_facet |
Antarc* Antarctic Sea ice |
op_doi |
https://doi.org/10.12770/1241fd87-dfc6-4be1-9bfe-7bc222f9d785 |
_version_ |
1778517399270588416 |