ERS-1 Radar Interferometry Over an Ice Stream in Northeast Greenland
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Engineering topics
Publications and source records attributed to Kwok, R..
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This paper presents a model to calculate the temperature dependence of effective permittivities for a heterogeneous anisotropic medium containing multiphase scatters. With the strong permittivity fluctuation approach, the model is developed to account for the electrodynamic scattering effect together with the quasi-static characteristics of multiple species and subspecies of inhomogeneities with distributed orientations, sizes, and shapes.
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Both topography and motion information are present in repeat pass ERS-1 interferograms over ice sheets.
We propose a Lagrangian ice motion tracker to follow the trajectory of ice particles at initially fixed grid points in the winter Arctic.
The backscatter signature of sea ice in newly-opened leads frequently overlaps with that of older and thicker ice types.
The directional orientations of leads in the winter ice pack of the Beaufort Sea are studied both spatially and temporally. Data from the European Earth Resources Satellite-1 (ERS-1) Synthetic Aperture Radar (SAR) was used. The SAR data was produced in image form at the Alaska SAR Facility (ASF) with 100 x 100 m pixel resolution. The lead ice pixels, which included all non-multiyear ice, were defined using a simple thresholding of the radar backscatter values. The orientations of the leads covering the Beaufort Sea during the period of January through March of 1992 were derived using a lead skeletonization technique. Results show a strong temporal persistence in the distribution and orientation of the leads during this period.
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We discuss the observed C- and L-band polarimetric signatures of thin lead ice in one Synthetic Aperture Radar image based on the expected ice properties and results from a scattering model.
This paper investigates the symmetry of polametric scattering and emission coefficients of media with reflection symmetry.
Physical, structural, and electromagnetic properties and interrelating processes in sea ice are used to develop a composite model for polarimetric backscattering signatures of sea ice.