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      • The sensitivity of synthetic aperture radar (SAR) polarization information to snow depth changes provides new opportunities for regional snow depth retrieval in mountains with thick snow cover. However, interference from soil signals can affect the accurate quantification of snow volume scattering signals.
      www.sciencedirect.com/science/article/pii/S1569843224002279
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  2. Apr 24, 2024 · soil signals can affect the accurate quanti cation of snow volume scattering signals. The aim of this study was to develop a dual-polarimetric radar snow depth estimation...

  3. 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.

  4. May 17, 2010 · However, a number of snow pack properties, including snow density, particle size, crystal shape, stratification, ground surface roughness and soil moisture, affect the microwave scattering signals and need to be properly modeled and exploited.

    • Jinyang Du, Jiancheng Shi, Jiancheng Shi, Helmut Rott
    • 2010
  5. Jul 4, 2022 · Microwave scattering by snow is reformulated as a function of snow physical and measurable variables only, without empirical adjustments. Two new metrics, microwave grain size and polydispersity, are introduced to describe the length scale complexity of the snow microstructure.

    • 3
    • 3, Issue4
    • 04 July 2022
  6. Table 3.1 parameter ℎ for the air/soil and snow/soil interface with rms height of 5 cm from L to Ku band. The effective permittivity of snow is 1.44 for snowpack with snow density 275 kg/m3 and grain size 1 mm. ..... 86

  7. This work demonstrates that the VS difference between 18 and 36 GHz is larger and the dependence of VS on grain size is weaker than those represented by existing methods. Volume scattering (VS) estimation plays a critical role in microwave emission modeling of the snowpack.

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