Read e-book online 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 ebook stories contemporary advances within the use of SAR imagery for operational functions and for helping technology investigations of the polar oceans. the real parameters that are extracted from spaceborne SAR imagery are mentioned. Algorithms utilized in such analyses are defined and knowledge platforms utilized in generating the ocean ice items are provided.

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

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5) more closely approximates the pattern of (To, suggesting that the snow volume may be having little or no effect relative to the ice surface on (TO during this period. In time series 2 Qco follows a similar pattern to cro while QCi appears to be nearly constant. It appears from this relationship that changes in the snow cover both affecting and affected by Qc o may be detected by the SAR, whereas QCi appears to be independent of the observed changes in (TO in time series 2. In general, as the conductive flux decreases there is a decrease in (TO.

A high dielectric change across any given interface means that the interaction will be dominated by surface scattering mechanisms. A small change in the dielectric constant across the interface will mean that a large proportion of energy will be transmitted across the interface and will be available for scattering within the volume. The dielectric constant of snow-covered sea ice is highly variable both temporally and spatially. Multiyear ice typically consists of a surface which has undergone an extensive process of recrystallization during the summer melt period.

The low net radiative values in 1992 were caused by persistent cloud cover, and frequent snowfall events. In general it appears that net radiation of the entire snow-iceocean system (Q*) reverses from being predominantly negative to being predominantly positive early in June or late May (between days 150 and 160) for the first-year ice sites. Once Q* becomes positive a rapid temporal increase is observed. This is associated with increasing water in liquid phase within the snowpack (Barber et al.

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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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