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  1. Polarimetric Synthetic Aperture Radar (PolSAR) can precisely describe the backscattering of the target and emerge as an effective tool for SD retrieval. The backscattering component of dry snow is mainly composed of volume scattering from the snowpack and surface scattering from the snow-ground interface.

  2. Jun 1, 2024 · This framework is based on the dual-polarimetric radar vegetation index (DpRVI c), which enhances the snow volume scattering signal and reduces soil interference by integrating soil purity and a conditioning factor to fully exploit the advantages of polarimetric SAR information.

  3. Nov 1, 2020 · In this study, we proposed a new method to retrieve snow wetness from full-polarimetric synthetic aperture radar (SAR) data. First, the dominant scattering components, i.e. surface and volume scattering, in wet-snow conditions were obtained by polarimetric decomposition.

    • Wei Ma, Pengfeng Xiao, Pengfeng Xiao, Xueliang Zhang, Yina Song, Tengyao Ma, Lizao Ye
    • 2020
  4. Jan 23, 2020 · Pivot indicated that the presence of short vegetation (height < 30 cm) does not significantly affect the backscatter from snow surfaces. Based on these observations, the range of H (1- A ) < 0.5 is very low for snow and bare soil surface, with the lower values indicating the presence of snow.

  5. Nov 25, 2014 · In the VIS, the volume scattering contribution to the reflected light is dominant since the light absorption by the ice is so small. The volume scattering contribution is typically due to multiple scattering implying that the reflected light is basically unpolarized.

  6. The effect of a densely packed medium in snow polarization was theoretically studied based on ray-tracing simulations [43] , and it was later confirmed by Lv and Sun [44] that the changes of the ...

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  8. Oct 11, 2019 · The co-polarized σ 0 vv measurements (Fig. 3, left column) show little variation throughout the winter, due to the limited absorption or scattering by dry snow in vv-polarization at C-band.

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