T. Hunewinkel et al., IMPROVED DETERMINATION OF THE SEA-ICE EDGE WITH SSM I DATA FOR SMALL-SCALE ANALYSES/, IEEE transactions on geoscience and remote sensing, 36(5), 1998, pp. 1795-1808
A method to derive the sea ice edges from the 37- and 85-GHz channels
of the spaceborne Special Sensor Microwave/Imager (SSM/I) with higher
resolution than operational ice concentration analyses is developed. A
combined ice-atmosphere model to evaluate atmospheric influences show
ed that under clear sky conditions the error of the ice edge position
is 3.1 km an average. The method performs well up to total liquid wate
r content (TWC) of 125 g/m(2) and overestimates the ice extent when TW
C increases up to 250 g/m(2). The algorithm is suitable to classify op
en water, the interior ice pack, and thin ice (nilas) or low ice conce
ntrations caused by a mixture of open water and pancake ice. Simulatio
ns showed that interpolation and resolution-matching techniques may im
prove the retrieval results with emphasis on interpolation, Validation
of the algorithm with high-resolution infrared data shows errors of t
he ice edge on average less than 5 km, Comparison with the NASA Team i
ce concentration algorithm in the Weddell Sea, Antarctica, shows best
agreement with the contour line of 33% ice concentration. The suitabil
ity of the method for mesoscale investigations is demonstrated with a
time series of a meander structure in the marginal ice zone (MIZ).