Professor Dr. Costas Tsatsoulis, Dr. Ronald Kwok (auth.)'s Analysis of SAR Data of the Polar Oceans: Recent Advances PDF

By Professor Dr. Costas Tsatsoulis, Dr. Ronald Kwok (auth.)

ISBN-10: 3642602827

ISBN-13: 9783642602825

ISBN-10: 3642643345

ISBN-13: 9783642643347

This booklet reports contemporary advances within the use of SAR imagery for operational purposes and for assisting technology investigations of the polar oceans. the real parameters which might be extracted from spaceborne SAR imagery are mentioned. Algorithms utilized in such analyses are defined and information platforms utilized in generating the ocean ice items are provided.

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Extra resources for Analysis of SAR Data of the Polar Oceans: Recent Advances

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3 GHz) from the snow volume during this period. Within first-year sea ice, microwave scattering appears to be dominated by a combination of basal layer volume scattering and ice surface scattering. During this period we would expect to find a significant difference in solar noon versus solar midnight observations, as small amounts of water in liquid phase would contribute to grain growth and the elevated temperatures would significantly increase the brine volume of the ice surface and snow basal layer.

The columnar-oriented crystals occur at deeper levels and are a result of the ice growing under the quiescent conditions of a frazil or shuga layer of new ice. G. BARBER, A. N. PAPAKYRIAKOU 30 ppt at the ice-ocean interface]. 96 g·cm-3• Liquid brine is interspersed through the ice as intercrystalline brine inclusions and brine drainage channels. The brine inclusions are generally formed in the orientation of growth (vertical) or directed according to the predominant ocean current (Vant et al. 1978).

11, 13, the image and output are characterized by fewer large floes, with an increased relative fraction of smaller floes and water/ice mixture as well. This follows the intuitive trend over the summer season of floes becoming smaller with melting, which is also reflected by the relative increase in water/ice mixture or subpixel size floes. Also, the bright open water provides good contrast with the surrounding ice and in this case is also segmented quite accurately. The algorithm has particular difficulty in at least two situations, when the radar signature of the ice pack is bright, and when analyzing imagery from the marginal ice zone.

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Analysis of SAR Data of the Polar Oceans: Recent Advances by Professor Dr. Costas Tsatsoulis, Dr. Ronald Kwok (auth.)

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