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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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41#
發(fā)表于 2025-3-28 18:38:34 | 只看該作者
Book 1998lemented and tested. One chapter is from the Alaskan SAR Facility, the major NASA archive of polar SAR data and a source of many SAR analysis algorithms, including high-level results of such analyses. One chapter has been written jointly by the US and Canadian Ice Centers, which provide e.g., operat
42#
發(fā)表于 2025-3-28 21:06:03 | 只看該作者
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發(fā)表于 2025-3-29 01:32:35 | 只看該作者
44#
發(fā)表于 2025-3-29 05:21:05 | 只看該作者
Direct and Large-Eddy Simulation Iover the period 1992 -1995, in conjunction with SAIC (Science and Engineering) and Scott Polar Research Institute, and three commercial polar operators (Nunaoil, Canarctic, and BP) with varying interests in the Arctic.
45#
發(fā)表于 2025-3-29 10:30:44 | 只看該作者
46#
發(fā)表于 2025-3-29 13:23:14 | 只看該作者
F. Ambrogi,U. Piomelli,D. E. Rivalhas been limited by a paucity of observational data. Satellite observations promise to illuminate many relationships and underpin new theoretical understanding. Seasonal transitions on Arctic sea ice are especially germane to studies of global climate and links between high latitude and global geophysical processes.
47#
發(fā)表于 2025-3-29 17:16:40 | 只看該作者
Mapping the Progression of Melt Onset and Freeze-Up on Arctic Sea Ice Using SAR and Scatterometry,has been limited by a paucity of observational data. Satellite observations promise to illuminate many relationships and underpin new theoretical understanding. Seasonal transitions on Arctic sea ice are especially germane to studies of global climate and links between high latitude and global geophysical processes.
48#
發(fā)表于 2025-3-29 23:43:48 | 只看該作者
Effect of?Variable Density on?Subgrid Scalessical properties of the volume. This results in an integrated system whereby hydrospheric and atmospheric forcings are linked with changes in the geophysical and electrical characteristics of the snow-covered sea ice volume.
49#
發(fā)表于 2025-3-30 00:13:52 | 只看該作者
50#
發(fā)表于 2025-3-30 06:39:16 | 只看該作者
R. Corsini,A. Cimarelli,E. Stalio can be estimated through spectral analysis and wave models. The wave-ice interaction models take into account the physical characteristics of the ice cover and the wave parameters to predict wave dispersion, attenuation, refraction, and possibly ice thickness (Liu et al. 1991,1992; Liu 1995).
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