Preprints
https://doi.org/10.5194/egusphere-2024-3164
https://doi.org/10.5194/egusphere-2024-3164
02 Jan 2025
 | 02 Jan 2025
Status: this preprint is open for discussion and under review for Atmospheric Measurement Techniques (AMT).

Simulations of Spectral Polarimetric Variables measured in rain at W-band

Ioanna Tsikoudi, Alessandro Battaglia, Christine Unal, and Eleni Marinou

Abstract. In this work, the T-matrix approach is exploited to produce simulations of spectral polarimetric variables (spectral differential reflectivity, sZDR, spectral differential scattering phase, sδHV and spectral differential correlation coefficient, sρHV) for observations of rain acquired from a slant-looking W-band cloud radar. The spectral polarimetric variables are simulated with two different methodologies, taking into account the instrument noise and the stochastic movement of the raindrops introduced by raindrop oscillations and by turbulence. The simulated results are then compared with rain Doppler spectra observations from a W band millimeter-wavelength radar for moderate rain rate conditions. Two cases, differing in levels of turbulence, are considered. While the comparison of the simulations to the measurements presents a reasonable agreement for equi-volume diameters less than 2.25 mm, large discrepancies are found in the amplitude (but not the position) of the maxima and minima of sZDR and, more mildly, of sδHV. This pinpoints at a general weakness of the raindrops approximation with spheroids for simulating radar backscattering properties at W-band.

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Ioanna Tsikoudi, Alessandro Battaglia, Christine Unal, and Eleni Marinou

Status: open (until 07 Feb 2025)

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Ioanna Tsikoudi, Alessandro Battaglia, Christine Unal, and Eleni Marinou
Ioanna Tsikoudi, Alessandro Battaglia, Christine Unal, and Eleni Marinou

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Short summary
The study simulates spectral polarimetric variables for raindrops as observed by a cloud radar. Raindrops are modelled as oblate spheroids and backscattering properties are computed via the T-matrix method including noise, turbulence and spectral averaging effects. When comparing simulations to measurements, differences on the amplitudes of polarimetric variables are noted. This shows the challenge of using simplified shapes to model raindrop polarimetric variables when moving to mm wavelengths.