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- W3048581204 abstract "ABSTRACT The impacts of the differential phase of incident radar waves ( ψ i ) on measured differential reflectivity ( Z DR ), differential phase, and correlation coefficient from ice cloud particles are presented for radars employing simultaneous transmission and reception of orthogonally polarized waves (SHV radar design). The maximal values of Z DR and the differential phase upon scattering ( δ ) from ice particles are obtained as functions of ψ i . It is shown that SHV δ from ice particles can exceed a dozen degrees whereas the intrinsic δ is of a few hundredths of a degree. In melting layers, the δ values from particles obeying the Rayleigh scattering law can be several degrees depending on ψ i so that, to explain such δ values, an assumption of resonance scattering is not necessary. The phase δ affects the estimation of specific differential phase ( K DP ) in icy media and, therefore, the phase δ should be measured. The radar differential phase upon transmission ψ t is a part of ψ i and, therefore, affects the δ values. A radar capability to alter ψ i by varying ψ t could deliver additional information about scattering media." @default.
- W3048581204 created "2020-08-18" @default.
- W3048581204 creator A5054850351 @default.
- W3048581204 date "2020-08-01" @default.
- W3048581204 modified "2023-09-24" @default.
- W3048581204 title "Impacts of the Phase Shift between Incident Radar Waves on the Polarization Variables from Ice Cloud Particles" @default.
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- W3048581204 doi "https://doi.org/10.1175/jtech-d-19-0197.1" @default.
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