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    A Forced Gravity Wave Model of Serf-Organizing Convection 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 023:;page 3528
    Author(s): Raymond, David J.
    Publisher: American Meteorological Society
    Abstract: A two-dimensional, hydrostatic, nonrotating numerical model with a cumulus paramelerizafion is developed to study the early stages of mesozcale convective systems. Amplifying, forced gravity waves occur when peneirative ...
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    Regulation of Moist Convection over the West Pacific Warm Pool 

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 022:;page 3945
    Author(s): Raymond, David J.
    Publisher: American Meteorological Society
    Abstract: The mechanisms that regulate moist convection over the warm tropical oceans are not well understood. One school of thought holds that convection is caused by the convergence of moisture, which in turn is produced by an ...
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    The Hadley Circulation as a Radiative–Convective Instability 

    Source: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 009:;page 1286
    Author(s): Raymond, David J.
    Publisher: American Meteorological Society
    Abstract: Hadley cell simulations over a tropical ocean are reported that suggest that the emission and absorption of thermal radiation by clouds plays an important role in the dynamics of the Hadley circulation. In particular, ...
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    A C Language-Based Modular System for Analyzing and Displaying Gridded Numerical Data 

    Source: Journal of Atmospheric and Oceanic Technology:;1988:;volume( 005 ):;issue: 004:;page 501
    Author(s): Raymond, David J.
    Publisher: American Meteorological Society
    Abstract: A system for analyzing and displaying gridded numerical data called Candis is described. The system is written in the C programming language, and is built on a standard way of representing such data. The analysis package ...
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    Simulation of an Air Mass Thunderstorm Using the Two-Scale Model 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 009:;page 2014
    Author(s): Raymond, David J.
    Publisher: American Meteorological Society
    Abstract: The two-scale model (Raymond, 1979) is used to simulate a well-documented Colorado thunderstorm. Good agreement is found with the early and middle stages of the storm life cycle. Intense vertical mixing in the early stages ...
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    Wave-CISK in Mass Flux Form 

    Source: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 010:;page 2561
    Author(s): Raymond, David J.
    Publisher: American Meteorological Society
    Abstract: A reformulation of wave-CISK shows that gravity waves generated by the divergence of cumulus mass fluxes am responsible for the forcing of further convection. When downdrafts are included, a new, non-propagating instability ...
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    A Wave-CISK Model of Squall Lines 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 012:;page 1946
    Author(s): Raymond, David J.
    Publisher: American Meteorological Society
    Abstract: The wave-CISK model of Raymond incorporating lag effects in the updraft and downdraft is implemented as an initial value problem in physical space. Examples of both midlatitude and tropical squall lines are successfully ...
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    Prescribed Heating of a Stratified Atmosphere as a Model for Moist Convection 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 011:;page 1101
    Author(s): Raymond, David J.
    Publisher: American Meteorological Society
    Abstract: The response of a stratified atmosphere to a steady, moving source of heat is explored as a tool for understanding organized, moist convection. The results are shown to depend strongly on the ratio of the vertical wavelength ...
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    A Model for Predicting the Movement of Continuously Propagating Convective Storms 

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 007:;page 1308
    Author(s): Raymond, David J.
    Publisher: American Meteorological Society
    Abstract: The predictions of propagation velocity made by a linear model of moist convective instability are compared with actual case studies of severe local storms. Excellent agreement between observation and theory is found for ...
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    Application of a Generalized “Impedance Relationship” to Mesoscale Convergence Lines 

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 010:;page 1894
    Author(s): Raymond, David J.
    Publisher: American Meteorological Society
    Abstract: An extension to the Gossard-Munk impedance relation, valid for large-amplitude, dissipative disturbances, is outlined. This new relation yields information on the dissipative properties of a convergence line if the associated ...
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