Sea Ice Thickness derived from merging of L-Band radiometry and radar altimeter derived sea ice thickness
'''Short description:'''
Global sea ice thickness from merged L-Band radiometer (SMOS ) and radar altimeter (CryoSat-2, Sentinel-3A/B) observations during freezing season between October and April in the northern hemisphere and April to October in the southern hemisphere. The SMOS mission provides L-band observations and the ice thickness-dependency of brightness temperature enables to estimate the sea-ice thickness for thin ice regimes. Radar altimeters measure the height of the ice surface above the water level, which can be converted into sea ice thickness assuming hydrostatic equilibrium.
'''DOI (product) :'''
https://doi.org/10.48670/moi-00125
Données et ressources
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For accessing native data and Analysis-ready Cloud-optimized data services, consult this STAC metadata endpointJSON Ouvrir
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For accessing native data and Analysis-ready Cloud-optimized data services, consult this STAC metadata endpointJSON Ouvrir
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Informations supplémentaires
| Étendue temporelle | 2010-04-11 – en cours |
|---|---|
| Date (creation) | 2024-11-26 |
| Statut | onGoing |
| Fréquence de mise à jour | daily |
| Langue des métadonnées | en |
| Licence | See Copernicus Marine Environment Monitoring Service Data commitments and licence at: http://marine.copernicus.eu/web/27-service-commitments-and-licence.php |
| Métadonnées sources | ISO 19115 XML |
| Dernière mise à jour | 2026-11-04 |
| Créé | 2026-11-04 |
| API | package_show |