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    Flow in Severe Thunderstorms Observed bu Dual-Doppler Radar 

    Source: Monthly Weather Review:;1977:;volume( 105 ):;issue: 001:;page 113
    Author(s): Brandes, Edward A.
    Publisher: American Meteorological Society
    Abstract: Dual-Doppler (S-band) radar observations are used to describe both the three-dimensional flow and a fife cycle of a severe thunderstorm on 6 June 1974. The primary updraft region was near a small mesocyclonic circulation ...
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    Relationships Between Radar-Derived Thermodynamic Variables and Tornadogenesis 

    Source: Monthly Weather Review:;1984:;volume( 112 ):;issue: 005:;page 1033
    Author(s): Brandes, Edward A.
    Publisher: American Meteorological Society
    Abstract: A methodology for obtaining pressure perturbations and buoyancy in thunderstorms observed with Doppler radar is described and applied to two tornadic thunderstorms. Extracted thermodynamic information is combined with ...
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    Vertical Vorticity Generation and Mesocyclone Sustenance in Tornadic Thunderstorms: The Observational Evidence 

    Source: Monthly Weather Review:;1984:;volume( 112 ):;issue: 011:;page 2253
    Author(s): Brandes, Edward A.
    Publisher: American Meteorological Society
    Abstract: Doppler radar observations concerning the generation of vertical vorticity in tornadic thunderstorms are documented for two case studies and the role of downdrafts in intensifying vertical vorticity is examined. The ...
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    Mesocyclone Evolution and Tornadogenesis: Some Observations 

    Source: Monthly Weather Review:;1978:;volume( 106 ):;issue: 007:;page 995
    Author(s): Brandes, Edward A.
    Publisher: American Meteorological Society
    Abstract: Updraft mesocyclones in tornado-producing thunderstorms form along convergent and cyclonically sheared boundaries that separate inflow air entering forward and rear storm quadrants. Maximum tangential flow resides in girding ...
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    Finestructure of the Del City-Edmond Tornadic Mesocirculation 

    Source: Monthly Weather Review:;1981:;volume( 109 ):;issue: 003:;page 635
    Author(s): Brandes, Edward A.
    Publisher: American Meteorological Society
    Abstract: Interrelationships among severe thunderstorm wind flow, tornado parent circulation and tornado are examined with dense single- and dual-Doppler radar observations from the Del City-Edmond, Oklahoma, storm of 20 May 1977. ...
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    Evolution and Structure of the 6–7 May 1985 Mesoscale Convective System and Associated Vortex 

    Source: Monthly Weather Review:;1990:;volume( 118 ):;issue: 001:;page 109
    Author(s): Brandes, Edward A.
    Publisher: American Meteorological Society
    Abstract: Observations collected during the Oklahoma?Kansas PRE-STORM experiment are used to document the evolution and structure of the mesoscale convective system (MCS) that occurred on 6?7 May 1985. The storm began when a short ...
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    Gust Front Evolution and Tornado Genesis as Viewed by Doppler Radar 

    Source: Journal of Applied Meteorology:;1977:;volume( 016 ):;issue: 004:;page 333
    Author(s): Brandes, Edward A.
    Publisher: American Meteorological Society
    Abstract: Doppler radar observations are utilized to describe the evolution of the severe thunderstorm updraft mesocyclone and its associated gust front. Tornadoes form within the elliptical mesocyclonic circulation, apparently along ...
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    Optimizing Rainfall Estimates with the Aid of Radar 

    Source: Journal of Applied Meteorology:;1975:;volume( 014 ):;issue: 007:;page 1339
    Author(s): Brandes, Edward A.
    Publisher: American Meteorological Society
    Abstract: Estimates of precipitation are improved when raingage observations are used to calibrate quantitative radar data as well as to estimate precipitation in areas without radar data. Estimated areal precipitation depth errors ...
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    Freezing-Level Estimation with Polarimetric Radar 

    Source: Journal of Applied Meteorology:;2004:;volume( 043 ):;issue: 011:;page 1541
    Author(s): Brandes, Edward A.; Ikeda, Kyoko
    Publisher: American Meteorological Society
    Abstract: A simple empirical procedure for determining freezing levels with polarimetric radar measurements is described. The algorithm takes advantage of the strong melting-layer signatures and the redundancy provided by the suite ...
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    Comparison of Polarimetric Radar Drop Size Distribution Retrieval Algorithms 

    Source: Journal of Atmospheric and Oceanic Technology:;2004:;volume( 021 ):;issue: 004:;page 584
    Author(s): Brandes, Edward A.; Zhang, Guifu; Vivekanandan, J.
    Publisher: American Meteorological Society
    Abstract: Recently, two physically based algorithms, the ?beta? (?) method and the ?constrained-gamma? method, have been proposed for retrieving the governing parameters of the gamma drop size distribution (DSD) from polarimetric ...
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