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    ADDITIONAL COMMENTS 

    Source: Journal of Meteorology:;1951:;volume( 008 ):;issue: 003:;page 204
    Author(s): Haltiner, G. J.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    UPPER-LEVEL VORTICES AND THE TURBULENT TRANSFER OF MOMENTUM 

    Source: Journal of Meteorology:;1951:;volume( 008 ):;issue: 003:;page 202
    Author(s): Haltiner, G. J.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    THE DIURNAL TEMPERATURE WAVE WITH A COEFFICIENT OF DIFFUSIVITY WHICH VARIES PERIODICALLY WITH TIME AND EXPONENTIALLY WITH HEIGHT 

    Source: Journal of Meteorology:;1958:;volume( 015 ):;issue: 003:;page 317
    Author(s): Haltiner, G. J.
    Publisher: American Meteorological Society
    Abstract: The partial differential equation for heat diffusion is numerically integrated by the Runge-Kutta method. Solutions are obtained for the diurnal temperature variation with a bounded coefficient of eddy diffusivity which ...
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    NUMERICAL PROGNOSIS INCLUDING NON-ADIABATIC WARMING 

    Source: Journal of Meteorology:;1960:;volume( 017 ):;issue: 002:;page 207
    Author(s): Haltiner, G. J.; Wang, Yeh-chum
    Publisher: American Meteorological Society
    Abstract: A model for numerical prediction of the 1000-mb surface is developed which includes a term expressing the interchange of sensible heat between the air and the underlying surface as well as the effect of terrain-induced ...
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    Some Recent Advances in Numerical Weather Prediction 

    Source: Monthly Weather Review:;1975:;volume( 103 ):;issue: 007:;page 571
    Author(s): Haltiner, G. J.; Williams, R. T.
    Publisher: American Meteorological Society
    Abstract: Recent developments in numerical weather prediction during the past several years are briefly summarized for the nonspecialist.
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    Computation of the Large Scale Vertical Velocity 

    Source: Journal of Applied Meteorology:;1963:;volume( 002 ):;issue: 002:;page 242
    Author(s): Haltiner, G. J.; Clarke, L. C.; Lawniczak, D. G.
    Publisher: American Meteorological Society
    Abstract: Vertical velocities are computed at four levels over a Northern Hemisphere grid in addition to a lower boundary value which is applied at terrain pressure and includes effects of frictionally- and terrain-induced vertical ...
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    NUMERICAL TROPOSPHERIC PREDICTION WITH A DIVERGENT BAROTROPIC MODEL 

    Source: Monthly Weather Review:;1963:;volume( 091 ):;issue: 005:;page 219
    Author(s): HALTINER, G. J.; NICHOLSON, HARRY E.; OAKES, WINSLOW B.
    Publisher: American Meteorological Society
    Abstract: An empirically adjusted equation based primarily on ?rnason's quasi-barotropic stratified model is used to predict the heights of the 300-, 500-, 700- and 850-mb. levels. The model shows moderate success and appears to ...
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    Minimal-Time Ship Routing 

    Source: Journal of Applied Meteorology:;1962:;volume( 001 ):;issue: 001:;page 1
    Author(s): Haltiner, G. J.; Hamilton, H. D.; ’Arnason, G.
    Publisher: American Meteorological Society
    Abstract: The effects of the state of the sea on the safety and economy of a ship's route are of considerable concern to the U. S. Navy and other organizations engaged in shipping. This article deals specifically with the problem ...
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    A PROPOSED METHOD FOR SHIP ROUTING USING LONG RANGE WEATHER FORECASTS 

    Source: Monthly Weather Review:;1968:;volume( 096 ):;issue: 005:;page 319
    Author(s): HALTINER, G. J.; BLEICK, W. E.; FAULKNER, F. D.
    Publisher: American Meteorological Society
    Abstract: Two advances in the calculus of variations method for minimal time ship routing are described. The first is a scheme for constructing ocean wave field forecasts which may be expected to have considerable skill for perhaps ...
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    HIGHER-ORDER GEOSTROPHIC WIND APPROXIMATIONS 

    Source: Monthly Weather Review:;1962:;volume( 090 ):;issue: 005:;page 175
    Author(s): ARNASON, G.; HALTINER, G. J.; FRAWLEY, M. J.
    Publisher: American Meteorological Society
    Abstract: Two iterative methods are described for obtaining horizontal winds from the pressure-height field by means of higher-order geostrophic approximations for the purpose of improving upon the geostrophic wind. The convergence ...
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