Observed relations between snowfall microphysics and triple‐frequency radar measurements

By S. Kneifel, A. Lerber, Jussi Tiira, D. Moisseev, Pavlos Kollias, Jussi Leinonen. 2015

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Confronting the Challenge of Modeling Cloud and Precipitation Microphysics (2020, background): “…the degree of resonance scattering (i.e., non‐Rayleigh scattering) for different radar frequencies allows for multifrequency scanning to yield further observational information (e.g., Bringi et al., 1986; Gaussiat et al., 2003; Kneifel et al., 2011, 2015; Kumjian et al., 2018; Tridon et al., 2017).”
A general database of hydrometeor single scattering properties at microwave and sub-millimetre wavelengths (2018, unknown): “The triple-frequency signatures have been shown to act as an indication of effective density, frequently linked to the degree of riming (Kneifel et al., 2015; Yin et al., 2017).”