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Characterization of L-band synthetic aperture radar (SAR) backscatter from floating and grounded thermokarst lake ice in Arctic Alaska

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Figure

Fig. 1. Network of Alaska and panelFigure 1: Study lakes are highlighted in yellow on a) northern Seward Peninsula (NSP) and b) Arctic Coastal 4 Plain (ACP) south of Barrow
Table 1. SAR data were selected based on data availability over two study areas for late March–April from 1993 through 2011.
Fig. 3. NSP, ERS-1, April 30, 1993) floating and grounded ice in late March–April are similar from year to year
Table 2. Summary of mean SAR backscatter intensity (dB) from floating and grounded lake ice for L- and C-bands from both study regions.
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