1999
DOI: 10.1175/1520-0426(1999)016<1900:pdpptf>2.0.co;2
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Polarization Diversity Pulse-Pair Technique for Millimeter-WaveDoppler Radar Measurements of Severe Storm Features

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Cited by 45 publications
(48 citation statements)
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“…The effect of cross polarization is to produce an interference signal in each copolar channel depending on the temporal shift between the H and V pair and the strength of the cross-polar power (which is given by the product of the LDR and the copolar power) and appear as ghost echoes (Battaglia et al 2013). The phases of ghost echoes are incoherent with respect to the echoes of interest and so do not bias the velocity estimates, but they increase their random error as a function of SGR (Pazmany et al 1999); as illustrated by the dashed lines in Fig. 3, when the SGR falls to 0 and −5 dB, this random error increases rapidly for shorter integration lengths.…”
Section: Potential Spurious Signals From the Doppler Radar Ground CLmentioning
confidence: 98%
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“…The effect of cross polarization is to produce an interference signal in each copolar channel depending on the temporal shift between the H and V pair and the strength of the cross-polar power (which is given by the product of the LDR and the copolar power) and appear as ghost echoes (Battaglia et al 2013). The phases of ghost echoes are incoherent with respect to the echoes of interest and so do not bias the velocity estimates, but they increase their random error as a function of SGR (Pazmany et al 1999); as illustrated by the dashed lines in Fig. 3, when the SGR falls to 0 and −5 dB, this random error increases rapidly for shorter integration lengths.…”
Section: Potential Spurious Signals From the Doppler Radar Ground CLmentioning
confidence: 98%
“…As explained in the "Why polarization diversity?" sidebar, WIVERN overcomes this dilemma by estimating the Doppler velocity using the polarization-diversity pulse-pair (PDPP) technique (Pazmany et al 1999) and would transmit a pair of pulses: one with horizontal polarization (H) and the other with vertical (V), with a short separation, T hv . A value of 20 μs is proposed for T hv so that the folding velocity is 40 m s −1 and large enough to comfortably exceed the errors of the winds calculated in the NWP models.…”
mentioning
confidence: 99%
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“…One efficient way to overcome the constraint imposed by (4) is to adopt a pulse polarization diversity strategy as described in [19,20]. On one hand, this choice increases the technological requirements and is subject to some limitations in its use, among them the fact that spectral processing could not be applied, hence narrowing the choice of spectral moment estimators to the Pulse Pair category.…”
Section: A Normalized Doppler Widthmentioning
confidence: 99%
“…The capability of building such a large statistics over the entire tropics and for all the stages of development of the convection would not only allow us to better quantify the various terms of the energy budget but also to improve convection parameterization relevant for cloud and climate model. Weather forecast 1 applications along with assimilation crave also use such dynamical information.…”
Section: Introductionmentioning
confidence: 99%