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Snow thickness retrieval over thick Arctic sea ice using SMOS satellite data

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Figure

Fig. 1. Brightness temperature at horizontal (blue) and vertical (ma-genta) polarisation for an incidence angle θ = 45◦ as a function ofice thickness for three different scenarios: (1) the solid lines showbrightness temperatures as modelled for snow-free sea ice; (2) thecircles show brightness temperatures as modelled for snow-free seaice with ice temperatures, as if the snow cover was present; and(3) the dashed lines show brightness temperatures as modelled forsnow-covered sea ice.
Table 1. The ice parameters r influencing the brightness temper-ature, their average values r (as used in Fig
Fig. 3. Horizontally polarised brightness temperature (incidence an-face temperature, ice salinity, or snow density, respectively
Table 2. Root mean square deviations RMSD, mean deviations MD,peratures and brightness temperatures as measured by SMOS forand coefficients of determination r2 for simulated brightness tem-horizontal and vertical polarisation.
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