An evaluation against on-ice buoy trajectories reveals that the RMSEs of the sea-ice drift CDR are small and vary with hemisphere and seasons (2.1 km for Arctic winters, 2.6 km for Arctic summer, 3 to 4 km for the Antarctic sea ice). The CDR is un-biased for Ar...
Sea ice motion from low-resolution satellite sensors: An alternative method and its validation in the Arctic EUMETSAT OSI SAF[1] The retrieval of sea ice motion with the Maximum Cross-Correlation (MCC) method from low-resolution (10芒聙聯15 km) spaceborne ... T Lavergne,S Eastwood,Z Teffa...