Sea-ice concentration is a low-resolution information layer for strategic planning purposes and to assist the interpretation of Sentinel-1 radar images. It is updated several times a day, automatically created and therefore to be used with care. Each pixel covers an area of 6.25 x 6.25 km2. Colours refer to the fractional area in percent (%) which is covered with ice. For a correct use of the sea-ice concentration layer the following guidelines should be considered:
Sea-ice concentration below ~10% is not resolved by the sensor. I.e. a region showing no sea-ice concentration can still have enough ice floes remaining a significant navigational hazard.
Close to the coast the sea-ice concentration is overestimated due to the influence of land You can best see this by looking on the Norwegian coast, which never has ice. The sea-ice concentration you see close to the Norwegian coast is the expected error for all coasts.
Sea-ice concentration does not indicate the type of ice. A 100% ice cover might be old multi-year ice, first-year ice or even a thin refrozen ice layer only. To clarify this, use additional radar images and/or ice charts, if available.
When you compare sea-ice concentration with a satellite image, be aware of the different time stamps. The time-stamp of the current sea-ice concentration layer is shown in the lower left corner in red letters just above the colour code legend. Usually sea-ice concentration is the newest layer.
Large atmospheric cyclones influence the measurements as well. Sometimes you see large areas indicating a sea-ice concentration of about 20-30 % in the middle of the open ocean. This is very likely an error due to a cyclone.
The sea-ice concentration data layer is an automatically generated product on the basis of satellite based passive microwave measurements provided by the Japanese Space Agencies AMSR2 sensor of the GCOM-W mission. The GCOM-W satellite circulates the earth 14.5 times a day (=14.5 revolutions per day). Due to its polar orbit, it crosses the poles during every revolution. The AMSR-E sensor records the passive microwave radiation on a stripe of 1450 km width (so called swath width). The data are thankfully provided by JAXA after every revolution, which enables so-called swath updates several times a day. The physical parameters of the GCOM-W mission are available here.
The conversion from passive microwave data to sea-ice concentration uses the ARTIST sea-ice algorithm from Spreen et al. (2008).