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On producing sea ice deformation data sets from SAR-derived sea ice motion

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Figure

Figure 1. Example of the divergence (a, c, e) and shear (b, d, f)obtained for the single-crack test case at a normalized resolutionof 0.1
Figure 3. Example of the unfiltered (left panel) and filtered (rightpanel) divergence obtained for the double-crack test case at a nor-malized resolution of 0.1
Figure 4. Unfiltered divergence rate computed from the RGPS seaice trajectory data set and corresponding to the pair of imagestaken at tk−1 = 3 February 2007 at 17:44:00 UTC and tk = 7 Febru-ary 2007 at 17:26:35 UTC.
Figure 6. Filtered divergence rate after the application of thesmoother to the selected cells (see Fig
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