By Professor Dr. Costas Tsatsoulis, Dr. Ronald Kwok (auth.)
This booklet experiences fresh advances within the use of SAR imagery for operational functions and for helping technological know-how investigations of the polar oceans. the $64000 parameters which are 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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Additional resources for Analysis of SAR Data of the Polar Oceans: Recent Advances
Int J Remote Sens 14: 295-311 Kwok R, Curlander JC, McConnell R, Pang SS (1991) An ice-motion tracking system at the Alaska SAR facility. IEEE J Ocean Eng 15, no 1: 44-54 Kwok R, Cunningham GF (1994) Backscatter characteristics of the winter ice cover in the Beaufort Sea. J Geophys Res 99: 7787-7802 Marr D, Hildreth E (1980) Theory of edge detection. Proc R Soc Lond B 207: 187-217 Matheron G (1975) Random sets and integral geometry. Wiley, New York Maykut GA, Perovich DK (1987) The role of shortwave radiation in the summer decay of a sea ice cover.
Although these patterns are undoubtedly frequency- and polarization-dependent it would appear that the C-VV manifestation for snow-covered 3 Role of SAR in Surface Energy Flux Measurements Over Sea Ice 43 -5 ,-------------__________________________- , ulliyear :::- -10 VJ ------ - - - - - - - '"- - - - 0::: " "- ~ 'b -IS " irst- Year [\ f I \ I \ I \ \ \ - \. 3. 1987. (Adapted from Barber et al. 1995) thick first-year and multiyear sea ice follows a form approximated in Fig_ 3. 1987) we can summarize the seasonal evolution of 0'0 as follows: Winter.
That component of the energy which is transmitted across the upper and lower interfaces is available within the volume to change the physical and electrical characteristics, which then cause changes in the flux proportions being reflected, transmitted or absorbed. This feedback mechanism creates a fundamental link between the physical properties of the marine cryosphere and the nature of electromagnetic interaction with the physical and electrical properties of the interface. In this chapter we present three sections through which we document our current understanding of how synthetic aperture radar (SAR) may be used in estimating components of the surface energy balance within the marine cryosphere.