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    Simulation of Radar Reflectivity and Surface Measurements of Rainfall 

    Source: Journal of Atmospheric and Oceanic Technology:;1987:;volume( 004 ):;issue: 003:;page 464
    Author(s): Chandrasekar, V.; Bringi, V. N.
    Publisher: American Meteorological Society
    Abstract: Raindrop size distributions (RSDs) are often estimated using surface raindrop sampling devices (e.g., disdrometers) or optical array (2D-PMS) probes. A number of authors have used these measured distributions to compute ...
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    Error Structure of Multiparameter Radar and Surface Measurements of Rainfall Part II: X-Band Attenuation 

    Source: Journal of Atmospheric and Oceanic Technology:;1988:;volume( 005 ):;issue: 006:;page 796
    Author(s): Chandrasekar, V.; Bringi, V. N.
    Publisher: American Meteorological Society
    Abstract: In Part II of this study, simulations of multiparameter radar observables to include X-band specific attenuation (A) are performed in order to study the relationship between A, Z, and ZDR. We also compute the triplet (A, ...
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    Error Structure of Multiparameter Radar and Surface Measurements of Rainfall Part I: Differential Reflectivity 

    Source: Journal of Atmospheric and Oceanic Technology:;1988:;volume( 005 ):;issue: 006:;page 783
    Author(s): Chandrasekar, V.; Bringi, V. N.
    Publisher: American Meteorological Society
    Abstract: Fluctuations in the radar measurements of ZDR are due to both signal power fluctuations and the cross-correlation between the horizontal and vertical polarized signals. In Part I of this study, these signals are simulated ...
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    Drop Axis Ratios from a 2D Video Disdrometer 

    Source: Journal of Atmospheric and Oceanic Technology:;2005:;volume( 022 ):;issue: 007:;page 966
    Author(s): Thurai, Merhala; Bringi, V. N.
    Publisher: American Meteorological Society
    Abstract: Results from an experiment to measure the drop shapes using a 2D video disdrometer (2DVD) are reported. Under calm conditions, drops were generated from a hose located on a bridge 80 m above ground, this height being ...
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    An Iterative Filtering Technique for the Analysis of Copolar Differential Phase and Dual-Frequency Radar Measurements 

    Source: Journal of Atmospheric and Oceanic Technology:;1995:;volume( 012 ):;issue: 003:;page 643
    Author(s): Hubbert, J.; Bringi, V. N.
    Publisher: American Meteorological Society
    Abstract: Copolar differential phase is composed of two components, namely, differential propagation phase and differential backscatter phase. To estimate specific differential phase KDP, these two phase components must first be ...
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    Application of the Generalized Gamma Model to Represent the Full Rain Drop Size Distribution Spectra 

    Source: Journal of Applied Meteorology and Climatology:;2018:;volume 057:;issue 005:;page 1197
    Author(s): Thurai, Merhala; Bringi, V. N.
    Publisher: American Meteorological Society
    Abstract: Abstract We report on measurements of drop size distributions (DSD) using collocated instruments (a Droplet Measurement Technologies, Inc., Meteorological Particle Spectrometer and a 2D-video disdrometer) from two locations ...
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    Evaluation of a New Polarimetrically Based Z–R Relation 

    Source: Journal of Atmospheric and Oceanic Technology:;2004:;volume( 021 ):;issue: 004:;page 612
    Author(s): Bringi, V. N.; Tang, Taiwen; Chandrasekar, V.
    Publisher: American Meteorological Society
    Abstract: A new polarimetrically based (or, pol-based) Z?R relation of the form Z = aR1.5 is described and evaluated where the multiplicative coefficient a is continuously adjusted as the drop size distribution evolves in space and ...
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    Multiparameter Radar Modeling and Observations of Melting Ice 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 005:;page 549
    Author(s): Vivekanandan, J.; Bringi, V. N.; Raghavan, R.
    Publisher: American Meteorological Society
    Abstract: This paper uses a microphysically detailed graupel and hail melting model, described by Rasmussen and Heymsfield, which is coupled to a radar model that computes multiparameter variables such as differential reflectivity, ...
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    On the Possible Use of Copolar Correlation Coefficient for Improving the Drop Size Distribution Estimates at C Band 

    Source: Journal of Atmospheric and Oceanic Technology:;2008:;volume( 025 ):;issue: 010:;page 1873
    Author(s): Thurai, M.; Hudak, D.; Bringi, V. N.
    Publisher: American Meteorological Society
    Abstract: A decrease in copolar correlation coefficient (?co) at C band has been observed for several rain events with broad drop size distributions (DSDs). Observational evidence comes from simultaneous measurements with a C-band ...
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    Dual-Polarization observations of Microbursts Associated with Intense Convection: The 20 July Storm during the MIST Project 

    Source: Monthly Weather Review:;1988:;volume( 116 ):;issue: 008:;page 1521
    Author(s): Wakimoto, Roger M.; Bringi, V. N.
    Publisher: American Meteorological Society
    Abstract: A detailed case study of the microbrust-producing storm on 20 July 1986 during the MIST Project is presented, together with visual (based on cloud photogrammetry) and radar observations during the life cycle of the storm. ...
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