ERS-1 Arctic daily sea ice extent and backscatter maps

The sea ice extent and normalized backscatter from the AMI scatterometer on ERS-1 result from the Bayesian discrimination of measured backscatter distances to prescribed ocean wind and sea ice geophysical model functions. The sea ice product contains the Bayesian sea ice probability and a proxy age...

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Bibliographic Details
Main Authors: Verhoef, Anton, Belmonte Rivas, Maria, Stoffelen, Ad
Format: Dataset
Language:unknown
Published: Royal Netherlands Meteorological Institute (KNMI) 2018
Subjects:
Online Access:https://dx.doi.org/10.21944/ers_1_nh_sea_ice_v1.0
https://scatterometer.knmi.nl/ice_extents/
id ftdatacite:10.21944/ers_1_nh_sea_ice_v1.0
record_format openpolar
spelling ftdatacite:10.21944/ers_1_nh_sea_ice_v1.0 2023-05-15T13:56:25+02:00 ERS-1 Arctic daily sea ice extent and backscatter maps Verhoef, Anton Belmonte Rivas, Maria Stoffelen, Ad 2018 application/x-netcdf https://dx.doi.org/10.21944/ers_1_nh_sea_ice_v1.0 https://scatterometer.knmi.nl/ice_extents/ unknown Royal Netherlands Meteorological Institute (KNMI) antarctic scatterometer sea ice extent radar backscatter ice age ice type ice class dataset Satellite data Dataset 2018 ftdatacite https://doi.org/10.21944/ers_1_nh_sea_ice_v1.0 2021-11-05T12:55:41Z The sea ice extent and normalized backscatter from the AMI scatterometer on ERS-1 result from the Bayesian discrimination of measured backscatter distances to prescribed ocean wind and sea ice geophysical model functions. The sea ice product contains the Bayesian sea ice probability and a proxy age of sea ice mapped onto 12.5 km polar stereographic grids. The sea ice extent is formed when the sea ice probability crosses a certain threshold, and the proxy age of sea ice is converted to (normalized VV C-band) sea ice backscatter using the instructions detailed in the User Manual. Dataset Antarc* Antarctic Arctic Sea ice DataCite Metadata Store (German National Library of Science and Technology) Antarctic Arctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic antarctic
scatterometer
sea ice extent
radar backscatter
ice age
ice type
ice class
spellingShingle antarctic
scatterometer
sea ice extent
radar backscatter
ice age
ice type
ice class
Verhoef, Anton
Belmonte Rivas, Maria
Stoffelen, Ad
ERS-1 Arctic daily sea ice extent and backscatter maps
topic_facet antarctic
scatterometer
sea ice extent
radar backscatter
ice age
ice type
ice class
description The sea ice extent and normalized backscatter from the AMI scatterometer on ERS-1 result from the Bayesian discrimination of measured backscatter distances to prescribed ocean wind and sea ice geophysical model functions. The sea ice product contains the Bayesian sea ice probability and a proxy age of sea ice mapped onto 12.5 km polar stereographic grids. The sea ice extent is formed when the sea ice probability crosses a certain threshold, and the proxy age of sea ice is converted to (normalized VV C-band) sea ice backscatter using the instructions detailed in the User Manual.
format Dataset
author Verhoef, Anton
Belmonte Rivas, Maria
Stoffelen, Ad
author_facet Verhoef, Anton
Belmonte Rivas, Maria
Stoffelen, Ad
author_sort Verhoef, Anton
title ERS-1 Arctic daily sea ice extent and backscatter maps
title_short ERS-1 Arctic daily sea ice extent and backscatter maps
title_full ERS-1 Arctic daily sea ice extent and backscatter maps
title_fullStr ERS-1 Arctic daily sea ice extent and backscatter maps
title_full_unstemmed ERS-1 Arctic daily sea ice extent and backscatter maps
title_sort ers-1 arctic daily sea ice extent and backscatter maps
publisher Royal Netherlands Meteorological Institute (KNMI)
publishDate 2018
url https://dx.doi.org/10.21944/ers_1_nh_sea_ice_v1.0
https://scatterometer.knmi.nl/ice_extents/
geographic Antarctic
Arctic
geographic_facet Antarctic
Arctic
genre Antarc*
Antarctic
Arctic
Sea ice
genre_facet Antarc*
Antarctic
Arctic
Sea ice
op_doi https://doi.org/10.21944/ers_1_nh_sea_ice_v1.0
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