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Estimating snow depth over Arctic sea ice from calibrated dual-frequency radar freeboards

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Figure

Table 1. AltiKa and CS-2 (SAR mode) operation characteristics.
Figure 1. The value �fAK, defined as the OIB laser freeboard mi-nus the AltiKa radar freeboard, plotted against AltiKa pulse peaki-ness, for the OIB spring campaigns of 2013 (red), 2014 (blue), and2015 (grey)
Figure 3. Monthly snow depths for the growth season November 2015 (a) to April 2016 (f), derived from the AltiKa minus CS-2 calibratedfreeboard
Figure 4. NSIDC November 2015 to April 2016 monthly mean sea ice drift vectors. Adapted from images retrieved from https://daacdata.apps.nsidc.org/pub/DATASETS/nsidc0116_icemotion_vectors_v3/browse/north/ (last access: 23 February 2018).
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