Titlebook: Analysis of SAR Data of the Polar Oceans; Recent Advances Costas Tsatsoulis,Ronald Kwok Book 1998 Springer-Verlag Berlin Heidelberg 1998 Cl

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N. Balcazar-Arciniega,J. Rigola,A. Olivaon, and thus requires the development of a variety of automated procedures. This is why the present chapter concentrates on the quantitative characterization of intermediate scale sea ice deformation.

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L. Schmitt,K. Richter,R. Friedrichhy periods of wind- and temperature-driven dynamic changes in the ice cover are accompanied by periods where the region is blanketed by cloud, and when the atmosphere is inherently more electromagnetically opaque. During storms, the probability with which the area is cloud covered is extremely high,

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Militia

Identifying Ice Floes and Computing Ice Floe Distributions in SAR Images,ets, for example. Forcing from wind and waves fractures the thickening ice into pieces or floes, which then collide with each other. Over a winter season, the resulting sea ice matrix consists of fairly rounded floes with deformed surfaces composed of ridges and hummocks, separated by open water are

晚间

Tartar

Extraction of Intermediate Scale Sea Ice Deformation Parameters from SAR Ice Motion Products,on this scale interact with both the climate scale (100-300 km) sea ice processes and floe scale (1 km) processes. Understanding the intermediate regional scale sea ice deformation can help bridge the gap between the sea ice behavior on the floe scale, which is in situ measurable, and the one on the

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慷慨援助

GIST

Mapping the Progression of Melt Onset and Freeze-Up on Arctic Sea Ice Using SAR and Scatterometry,as a wide range of human activities. In remote parts of the world, including the Arctic, knowledge and understanding of annual and interannual cycles has been limited by a paucity of observational data. Satellite observations promise to illuminate many relationships and underpin new theoretical unde