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    Observational Analysis of a Gust Front to Bore to Solitary Wave Transition within an Evolving Nocturnal Boundary Layer 

    Source: Journal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 008:;page 2016
    Author(s): Knupp, Kevin
    Publisher: American Meteorological Society
    Abstract: The evolution of a gust front to bore to solitary wave transition, and comprehensive information on the evolving nocturnal boundary layer (NBL) associated with this change, are described with analysis of radar and profiler ...
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    Downdrafts within High Plains Cumulonimbi. Part II: Dynamics and Thermodynamics 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 024:;page 3965
    Author(s): Knupp, Kevin R.
    Publisher: American Meteorological Society
    Abstract: The dynamical and thermodynamical properties of precipitation-associated downdrafts are examined using a Lagrangian trajectory analysis approach applied to parcels passing through the low-level downdraft of precipitating ...
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    Observed Characteristics of the Afternoon–Evening Boundary Layer Transition Based on Sodar and Surface Data 

    Source: Journal of Applied Meteorology and Climatology:;2011:;volume( 051 ):;issue: 003:;page 571
    Author(s): Busse, Jessica; Knupp, Kevin
    Publisher: American Meteorological Society
    Abstract: he early-evening boundary layer transition has been defined in the past using a variety of criteria, the most popular of which is the onset of a negative surface heat flux. According to this definition, the transition is ...
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    Downdrafts within High Plains Cumulonimbi. Part I: General Kinematic Structure 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 006:;page 987
    Author(s): Knupp, Kevin R.
    Publisher: American Meteorological Society
    Abstract: This paper presents results from a comprehensive investigation in which observations from several case studies an integrated with three-dimensional cloud model results to examine the general kinematic structure of downdrafts ...
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    Radar and Profiler Analysis of Colliding Boundaries: A Case Study 

    Source: Monthly Weather Review:;2009:;volume( 137 ):;issue: 007:;page 2203
    Author(s): Karan, Haldun; Knupp, Kevin
    Publisher: American Meteorological Society
    Abstract: The kinematics of a head-on collision between two gust fronts, followed by a secondary collision between a third gust front and a bore generated by the initial collision, are described using analyses of Weather Surveillance ...
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    Structure and Evolution of a Long-Lived, Microburst-Producing Storm 

    Source: Monthly Weather Review:;1996:;volume( 124 ):;issue: 012:;page 2785
    Author(s): Knupp, Kevin R.
    Publisher: American Meteorological Society
    Abstract: This paper describes an analysis of a long-lived, microburst-producing storm that evolved within a relatively dry environment having a relatively low CAPE value of 450 J kg?1. The storm displayed a variety of kinematic and ...
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    Numerical Simulation of Low-Level Downdraft Initiation within Precipitating Cumulonimbi: Some Preliminary Results 

    Source: Monthly Weather Review:;1989:;volume( 117 ):;issue: 007:;page 1517
    Author(s): Knupp, Kevin R.
    Publisher: American Meteorological Society
    Abstract: Two three-dimensional cloud model simulations are examined and compared in order to define some of the characteristics of the low-level downdraft initiation process within deep precipitating convection. The initial environment ...
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    Mobile Integrated Profiler System (MIPS) Observations of Low-Level Convergent Boundaries during IHOP 

    Source: Monthly Weather Review:;2006:;volume( 134 ):;issue: 001:;page 92
    Author(s): Karan, Haldun; Knupp, Kevin
    Publisher: American Meteorological Society
    Abstract: Characteristics of convergent boundary zones (CBZs) sampled by the Mobile Integrated Profiling System (MIPS) during the 2002 International H2O Project (IHOP_2002) are presented. The MIPS sensors (915-MHz wind profiler, ...
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    Precipitation Growth Trajectories in a CCOPE Storm 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 011:;page 1057
    Author(s): Knight, Charles A.; Knupp, Kevin R.
    Publisher: American Meteorological Society
    Abstract: The growth trajectories of precipitation particles that attain diameters from 0.5 to 2.0 cm are modeled within the wind field of a small, relatively steady-state, southeastern Montana thunderstorm. The trajectories are ...
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    An Intense, Quasi-Steady Thunderstorm over Mountainous Terrain. Part II: Doppler Radar Observations of the Storm Morphological Structure 

    Source: Journal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 002:;page 343
    Author(s): Knupp, Kevin R.; Cotton, William R.
    Publisher: American Meteorological Society
    Abstract: An analysis of an intense, quasi-steady thunderstorm which developed over mountainous terrain is presented. This storm, extensively analyzed using multiple Doppler radar and surface mesonet data, formed within an environment ...
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