2014
DOI: 10.1175/jtech-d-13-00231.1
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Experimentally Based Estimates of Relations between X-Band Radar Signal Attenuation Characteristics and Differential Phase in Rain

Abstract: Correcting observed polarimetric radar variables for attenuation and differential attenuation effects in rain is important for meteorological applications involving measurements at attenuating frequencies such as those at X band. The results of estimating the coefficients in the correction-scheme relations from dual-wavelength polarimetric radar measurements of rainfall involving attenuating and nonattenuating frequencies are described. Such coefficients found directly from measurements are essentially free fr… Show more

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Cited by 10 publications
(13 citation statements)
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“…In Equation 3, Φ DP (X) − Φ DP (0) is a continuously increased X band differential phase value with increasing range and Φ DP (0) (unit: deg) is the estimated initial system phase at each radial due to radar hardware [11,14]. The reflectivity difference ∆Z(S-X) between S and X band pixels in the same space-time, with approximately equal horizontal distances and heights, is approximately equal to the X band PIA at horizontal polarization.…”
Section: Of 16mentioning
confidence: 99%
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“…In Equation 3, Φ DP (X) − Φ DP (0) is a continuously increased X band differential phase value with increasing range and Φ DP (0) (unit: deg) is the estimated initial system phase at each radial due to radar hardware [11,14]. The reflectivity difference ∆Z(S-X) between S and X band pixels in the same space-time, with approximately equal horizontal distances and heights, is approximately equal to the X band PIA at horizontal polarization.…”
Section: Of 16mentioning
confidence: 99%
“…3. Results Table 2 lists the values of ratio a found through theoretical simulations assuming a mean drop aspect ratio (i.e., minor-to-major dimension ratio) vs. size relations and measured rain temperature in the radar site and using the measurements of the dual-wavelength radar with dual-polarization capabilities introduced by Matrosov et al, 2014 [11]. From Table 2, it can be seen that the values of ratio a generally vary in the range from 0.1 to 0.3.…”
Section: (B) Collections Of Pixel Pairs Between X and S Bandsmentioning
confidence: 99%
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“…The common polarimetric approach for compensating rain path attenuation is based on the assumed linearity between specific attenuation as well as differential attenuation and specific differential phase (Bringi et al, 1990;Testud et al, 2000), i.e., A H,DP = γ H,DP K DP . It is known that the coefficients γ H,DP are variable, depending on raindrop size, shape and temperature (Jameson, 1992;Matrosov et al, 2014). Despite the fact that several optimization approaches have been proposed (Carey et al, 2000;Vulpiani et al, 2008), solutions that are totally reliable for operational applications are not yet available.…”
Section: G Vulpiani Et Al: Characterization Of Mediterranean Hail-bmentioning
confidence: 99%