Arctic sea ice freeboard and thickness from data of the European radar altimeter CryoSat-2 is generated by the Alfred Wegener Institute (AWI) in the winter month (October-April). The resulting data products are publicly available under a  Creative Commons Attribution 4.0 International (CC BY 4.0) license. Please read the documentation below for data access and formats.

Sea ice thickness information from CryoSat-2 is available from two data streams

  1. near-real time (nrt) data with a delay of 2 days
  2. reprocessed data with a delay of 31 days


Hendricks, S. and Ricker, R. (2019): Product User Guide & Algorithm Specification: AWI CryoSat-2 Sea Ice Thickness (version 2.1), Technical Report, hdl:10013/epic.7dacf2fe-bead-4a1b-a266-c4fdd022877f, https://epic.awi.de/id/eprint/49542/


This service does not intent to be an operational data dissimination service. Interruptions of data provision might occur at any time. We stress the fact that the interpretation of CryoSat-2 radar signals over sea ice and the uncertainties of freeboard retrieval and conversion into sea ice thickness are still an active field of research. This product shall therefore be used as a tool for the scientific community to enable further development of sea ice thickness retrieval algorithms from radar altimetry.

It is however our aim, to regurlary revise and improve the sea-ice processing chain for CryoSat-2 data and provide incremental update at the start of each Arctic winter season in October.

We encourage users to give feedback at info(at)meereisportal.de for further improvements of the AWI CryoSat-2 sea ice product.


Data Access


Data Content & Format


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Acknowledgements



Cryosat-2 Level-1 data is courtesy of the European Space Agency
ESA CryoSat website
ESA CryoSat-2 Wiki






Sea ice concentration and type data is courtesy of the Ocean and Sea Ice Satellite Application Facility (OSI-SAF)






Global mean sea surface products (DTU15/DTU18) is courtesy of the Danish National Space Institute (DTU Space)






Snow depth from AMSR2 is courtesy of the Institute for Environmental Physics of the University Bremen