Open AccessParameters of Cloud Ice Particles Retrieved from Radar Data
Author(s) -
Valery Melnikov
Publication year - 2017
Publication title -
journal of atmospheric and oceanic technology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.774
H-Index - 124
eISSN - 1520-0426
pISSN - 0739-0572
DOI - 10.1175/jtech-d-16-0123.1
Subject(s) - radar , remote sensing , orientation (vector space) , physics , polarimetry , geology , optics , computer science , geometry , scattering , mathematics , telecommunications
The mean axis ratio (length/width) and the degree of orientation of cloud ice particles are retrieved from radar differential reflectivity ( Z DR ) and the copolar correlation coefficient ( ρ hv ) measured with the S-band WSR-88D radar. Hardware differential phases and amplifications in the polarimetric channels affect measured Z DR and ρ hv and are taken into consideration in the retrieval procedure. The retrieval is performed for particles in shapes of hexagonal prisms, which are closer to shapes of real cloud particles than frequently used spheroids. The median retrieved axis ratio for prisms is larger than that for spheroids. The statistical 1 σ retrieval errors caused by fluctuations of radar returns are about 40% in areas of signal-to-noise ratios stronger than 10 dB. The values of the degree of orientation lie in an interval from 2° to 23°, which points to significant perturbations in the orientations of ice particles most likely caused by the wind field.