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An Inter-Comparison of Techniques for Determining Velocities of Maritime Arctic Glaciers, Svalbard, Using Radarsat-2 Wide Fine Mode Data

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Academic year: 2020

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Figure 1. Image extents of Radarsat-2 image pairs utilized in this study (green outlines denote Radarsat-2 imagery with acquisition dates)
Table 1. Radarsat-2 Beam modes used in this study with nominal resolution and scene size
Figure 2. Comparison of displacements of Kronebreen from RS-2 Wide Fine data and GPS. (a) RS-2 Wide Fine (GAMMA) vs
Figure 3. Surface speed of Svalbard glaciers processed with the GRAY method (fastest speed is quoted)
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