57A198
Sea-ice freeboard, snow depth and sea-ice roughness in East
Antarctica from in situ and multiple satellite data
Thorsten Markus, Robert Massom, Anthony Worby, Nathan
Kurtz
Corresponding author: Thorsten Markus –
thorsten.markus@nasa.gov
In October 2003 a campaign onboard the Australian
icebreaker Aurora Australis had the
objective to validate standard Aqua Advanced Microwave Scanning Radiometer
(AMSR-E) sea-ice products. Additionally, the satellite laser altimeter on Ice,
Cloud and land Elevation Satellite (ICESat) was in operation. The capture
large-scale information of the sea-ice conditions as necessary for satellite
validation, the measurement strategy, therefore, was to obtain large-scale
sea-ice statistics using extensive sea-ice measurements in a Lagrangian
approach. A drifting buoy array spanning initially 50 km × 100 km was
surveyed extensively using 50–500 m transects as well as performing random
sampling within the buoy array using helicopters. Extrapolation using buoy drift
information was utilized to enhance the data volume in time. The results show
that ICESat freeboard estimates have a mean difference of 1.8 cm when compared
with the in situ data and a correlation coefficient of 0.6. Furthermore,
incorporating ICESat roughness information into the AMSR-E snow-depth algorithm
significantly improves snow-depth retrievals.
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