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Aliasing in Micro Rain Radar data due to strong vertical winds

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Figure

Figure 2. Time evolution of the spectral reflectivity as a function of the Doppler velocity, at (a) 100 m, (b) 300 m, (c) 500 m, and (d) 700 m AGL
Table 1. Radar Reflectivity Factor Z, Rainrate R, and Attenuation Coefficient k Calculated From the Aliased and Corrected DSDs of Figure 3b

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