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    On Mountain Upslope Winds 

    Source: Journal of the Atmospheric Sciences:;1964:;Volume( 021 ):;issue: 006:;page 622
    Author(s): Orville, Harold D.
    Publisher: American Meteorological Society
    Abstract: Equations developed by Ogura (1962) for a two dimensional axially symmetric thermal initiation problem are adjusted to two rectilinear dimensions and used in a numerical study of mountain upslope winds. The winds are ...
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    A Numerical Study of the Initiation of Cumulus Clouds over Mountainous Terrain 

    Source: Journal of the Atmospheric Sciences:;1965:;Volume( 022 ):;issue: 006:;page 684
    Author(s): Orville, Harold D.
    Publisher: American Meteorological Society
    Abstract: The initiation of cumulus clouds over mountainous terrain is investigated by means of a numerical model. Two-dimensional motion is simulated over a mountain and valley. Changes at the mountain surface of both temperature ...
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    A Photogrammetric Study of the Initiation of Cumulus Clouds over Mountainous Terrain 

    Source: Journal of the Atmospheric Sciences:;1965:;Volume( 022 ):;issue: 006:;page 700
    Author(s): Orville, Harold D.
    Publisher: American Meteorological Society
    Abstract: The initiation of cumulus clouds over mountainous terrain is investigated photogrammetrically. Stereo pairs taken at one- and two-minute intervals are analyzed for four days of cumulus initiation over the Santa Catalina ...
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    Comments on “Cloud Interaction and Merging on Day 261 of GATE” 

    Source: Monthly Weather Review:;1984:;volume( 112 ):;issue: 002:;page 387
    Author(s): Orville, Harold D.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Grid Interval Effects on a Numerical Model of Upslope Winds and Mountain-Induced Cumulus 

    Source: Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 006:;page 1164
    Author(s): Orville, Harold D.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Comment on “Effects of the Pressure Perturbation Field in Numerical Models of Unidirectionally Sheared Thunderstorm Convection: Two Versus Three Dimensions” 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 020:;page 2220
    Author(s): Orville, Harold D.
    Publisher: American Meteorological Society
    Abstract: No Abstract.
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    Comments on “Accuracy of Finite-Difference Methods Applied to the Advection Equation” 

    Source: Journal of Applied Meteorology:;1968:;volume( 007 ):;issue: 005:;page 938
    Author(s): Orville, Harold D.
    Publisher: American Meteorological Society
    Abstract: tract
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    A Review of Cloud Modeling in Weather Modification 

    Source: Bulletin of the American Meteorological Society:;1996:;volume( 077 ):;issue: 007:;page 1535
    Author(s): Orville, Harold D.
    Publisher: American Meteorological Society
    Abstract: The numerical modeling of clouds has a history almost as long as the modern-day concepts of the seeding of clouds. The various models and theoretical developments emerging from the model results are reviewed in this paper. ...
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    Comments on “Estimate of Precipitation Enhancement Potential for the Duero Basin of Spain” 

    Source: Journal of Applied Meteorology:;1990:;volume( 029 ):;issue: 002:;page 188
    Author(s): Orville, Harold D.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    On the Freezing of Liquid Water in a Cloud 

    Source: Journal of Applied Meteorology:;1973:;volume( 012 ):;issue: 004:;page 671
    Author(s): Orville, Harold D.; Hubbard, Kenneth
    Publisher: American Meteorological Society
    Abstract: A technique due to Saunders is used to give quantitative information on the amount of heating to be realized from the freezing of liquid water in a cloud. The commonly accepted value of ?C per gram of water frozen per ...
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