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Keywords |
Antarctica, Brightness temperature, Dome C, Ice, L-band, L-band brightness temperature, L-band characteristics, Microwave, SMOS observations, Scattering, Snow, Temperature measurement, brightness suggest snowpack, emission e-folding depth, hydrological techniques, incidence angles, ocean waves, radiative transfer, radiative transfer (RT) theory, radiative transfer theory, remote sensing, seasonal variations, snow, snow emission stability, snow properties, snowpack variability density, soil, soil moisture ocean salinity satellite observation, wave approach, wave theory, |
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Abstract |
Two electromagnetic models were used to simulate snow emission at L-band from in situ measurements of snow properties collected at Dome C in Antarctica. Two different approaches were used: one based on the radiative transfer theory and the other on the wave approach. The soil moisture ocean salinity (SMOS) satellite observations performed at 1.4 GHz (21 cm) were used to check the validity of these models. Model results based on the wave approach were in good agreement with SMOS observations, particularly for incidence angles lower than 55°. Comparisons suggest that the wave approach is more suitable to simulate brightness temperature at L-band than the transfer radiative theory, because interference between the layers of the snowpack is better taken into account. The model based on the wave approach was then used to investigate several L-band characteristics at Dome C. The emission e-folding depth, i.e., 67% of the signal, was estimated at 250 m, and 99% of the signal emanated from the top 900 m. L-band brightness temperature is only slightly affected by seasonal variations in surface temperature, confirming the high temporal stability of snow emission at low frequency. Sensitivity tests showed that good knowledge of density variability in the snowpack is essential for accurate simulations in L-band. |
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