Abstract
This study reports on four consecutive winter campaigns (2016 – 2020) at the “Davos-Laret Remote Sensing Field Laboratory” in the Swiss Alps to gain insight into the L-band microwave emission of ground covered with seasonal snow. Close-range L-band Brightness temperatures <inline-formula><tex-math notation="LaTeX">$T_\mathrm{{B}}^{p,\phi }(\theta)$</tex-math></inline-formula> were measured over the site scanning different observation nadir angles <inline-formula><tex-math notation="LaTeX">$\theta$</tex-math></inline-formula> and azimuth angles <inline-formula><tex-math notation="LaTeX">$\phi$</tex-math></inline-formula> at Horizontal and Vertical polarizations <i>p</i> = {H,V}. State parameters of the snowpack (e.g., height, density, SWE) and the subnivean soil (permittivity, temperature) were measured quasi-simultaneously using in-situ sensors and sampling, as well as meteorological data. In each campaign <inline-formula><tex-math notation="LaTeX">$T_\mathrm{{B}}^{p,\phi }(\theta)$</tex-math></inline-formula> were measured over a “natural area” and a “reflector area” with a metal mesh reflector laid on the ground before snow accumulation. The radiometer measurements over “reflector area” allowed to retrieve the time-series of Snow liquid Water-Content <inline-formula><tex-math notation="LaTeX">$W_\mathrm{{S}}$</tex-math></inline-formula> and Snow liquid Water-Column <inline-formula><tex-math notation="LaTeX">$WC_\mathrm{{S}}$</tex-math></inline-formula> which are employed as “derived measurements” to support interpretation of <inline-formula><tex-math notation="LaTeX">$T_\mathrm{{B}}^{p,\phi }(\theta)$</tex-math></inline-formula> measured over “natural areas” during different Winter phases. The detailed approach for the estimation of <inline-formula><tex-math notation="LaTeX">$W_\mathrm{{S}}$</tex-math></inline-formula> and <inline-formula><tex-math notation="LaTeX">$WC_\mathrm{{S}}$</tex-math></inline-formula> using L-band radiometer data is presented. The data and analyses in this paper address the following major points: i) Determination of the characteristic features of measured <inline-formula><tex-math notation="LaTeX">$T_\mathrm{{B}}^{p,\phi }(\theta)$</tex-math></inline-formula> during different periods in each of the four winter campaigns; ii) effects of dry- and wet snow precipitation on L-band radiometer data compared to corresponding simulations; iii) effect of removal and compression of the snowpack on <inline-formula><tex-math notation="LaTeX">$T_\mathrm{{B}}^{p,\phi }(\theta)$</tex-math></inline-formula>; and iv) effects of spatial heterogeneity on brightness temperatures. Finally, the study is concluded with recommendations relevant for future close-range remote sensing campaigns.
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