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    Radar Polarimetric Backscattering Properties of Conical Graupel 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 011:;page 1887
    Author(s): Aydin, K.; Seliga, T. A.
    Publisher: American Meteorological Society
    Abstract: Conical graupel is modeled using sphere-cone-oblate spheroidal shapes for the purpose of computing their backscattering properties at a wavelength of 10 cm in terms of the radar polarimetric observables, reflectivity ...
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    Disdrometer Measurements during an Intense Rainfall Event in Central Illinois: Implications for Differential Reflectivity Radar Observations 

    Source: Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 006:;page 835
    Author(s): Seliga, T. A.; Aydin, K.; Direskeneli, H.
    Publisher: American Meteorological Society
    Abstract: Empirical relationships for estimating rainfall rate, liquid water content and median volume diameter from radar measurements of reflectivity factor and differential reflectivity are derived from a disdrometer record of a ...
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    Remote Sensing of Hail with a Dual Linear Polarization Radar 

    Source: Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 010:;page 1475
    Author(s): Aydin, K.; Seliga, T. A.; Balaji, V.
    Publisher: American Meteorological Society
    Abstract: A technique for the remote sensing of hail with an S-band dual linear polarization radar is described. The method employs a new hail signal HDR, which is derived from disdrometer measurements of raindrop size distributions. ...
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    Potential Use of Radar Differential Reflectivity Measurements at Orthogonal Polarizations for Measuring Precipitation 

    Source: Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 001:;page 69
    Author(s): Seliga, T. A.; Bringi, V. N.
    Publisher: American Meteorological Society
    Abstract: The potential use of differential reflectivity measurements at orthogonal polarizations to determine rain-fall rate is examined. The method involves measurements of ZH and ZV, the radar reflectivity factors due to horizontally ...
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    A Differential Reflectivity Radar Hall Measurement Technique: Observations during the Denver Hailstorm of 13 June 1984 

    Source: Journal of Atmospheric and Oceanic Technology:;1990:;volume( 007 ):;issue: 001:;page 104
    Author(s): Aydin, K.; Zhao, Y.; Seliga, T. A.
    Publisher: American Meteorological Society
    Abstract: A differential reflectivity radar technique for observing hailstorms is demonstrated using measurements obtained during the 13 June 1984 Denver hailstorm. The hail regions of the storm are identified with the differential ...
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    Effects of Raindrop-Size Distribution Variation within the Radar Scattering Volume on Radar Observables 

    Source: Journal of Atmospheric and Oceanic Technology:;1990:;volume( 007 ):;issue: 006:;page 919
    Author(s): Scarchilli, G.; Gorgucci, E.; Seliga, T. A.; Aydin, K.
    Publisher: American Meteorological Society
    Abstract: Dual linear polarization weather radars measure as primary observables the mean power P?H, and P?V, corresponding to returns at horizontal and vertical polarizations, respectively. Differential reflectivity ZDR is defined ...
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    A Preliminary Study of Comparative Measurements of Rainfall Rate Using the Differential Reflectivity Radar Technique and a Raingage Network 

    Source: Journal of Applied Meteorology:;1981:;volume( 020 ):;issue: 011:;page 1362
    Author(s): Seliga, T. A.; Bringi, V. N.; Al-Khatib, H. H.
    Publisher: American Meteorological Society
    Abstract: Radar measurements of average rainfall rate over two separate 550 km2 areas am compared with raingage measurements in the same areas over time intervals of ?1 h. The measurements were performed to test the differential ...
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    Rainfall and Clutter Discrimination by Means of Dual-linear Polarization Radar Measurements 

    Source: Journal of Atmospheric and Oceanic Technology:;1991:;volume( 008 ):;issue: 006:;page 777
    Author(s): Giuli, D.; Gherardelli, M.; Freni, A.; Seliga, T. A.; Aydin, K.
    Publisher: American Meteorological Society
    Abstract: The presence of undetected mixed-phase precipitation or superimposed intense clutter can cause serious errors in the estimation of rainfall rate and other parameters of precipitation occurring in the radar scattering volume. ...
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