Recherche en Prévision Numérique (RPN): References
[1]Ritchie, H., 1985: Application of a
semi-Lagrangian integration scheme to the moisture equation in a regional
forecast model. Mon. Wea. Rev., 113, 424-435.[2]Ritchie, H., 1986: Eliminating the interpolation associated with the semi-Lagrangian scheme. Mon. Wea. Rev., 114, 135-146.
[3]Ritchie, H., 1987: Semi-Lagrangian advection on a Gaussian grid. Mon. Wea. Rev., 15, 608-619.
[4]Ritchie, H., 1988: Application of the semi-Lagrangian method to a spectral model of the shallow water equations. Mon. Wea. Rev., 116, 1587-1598.
[5]Ritchie, H., 1991: Application of the semi-Lagrangian method to a multilevel spectral primitive-equations model. Q.J. Royal Meteor. Soc., 117, 91-106.
[6]Beland, M., and C. Beaudoin, 1985: A global spectral model with a finite element formulation for the vertical discretization: adiabatic formulation. Mon. Wea. Rev., 113, 1910-1919.
[7]Benoit, R., J. Cote, and J. Mailhot, 1989: Inclusion of a TKE boundary layer parameterization in the Canadian regional finite-element model. Mon. Wea. Rev., 117, 1726-1750.
[8]Machenhauer, B., 1977: On the dynamics of gravity oscillations in a shallow water model with applications to normal mode initialization. Beitr. Phys. Atmos., 50, 253-271.
[9]Asselin, R., 1972: Frequency filter for time integrations. Mon. Wea. Rev., 100, 487-490.
[10]Mailhot, J., and R. Benoit, 1982: A finite-element model of the atmospheric boundary layer suitable for use with numerical weather prediction models. J. Atmos. Sci., 39, 2249-2266.
[11]McFarlane, N.A., 1987: The effect of orographically excited gravity-wave drag on the circulation of the lower stratosphere and troposphere. J. Atmos. Sci., 44, 1775-1800.
[12]Kita, K., and A. Sumi, 1986: Reference ozone models for middle atmosphere. Meteorological Research Report 86-2, Division of Meteorology, Geophysical Institute, University of Tokyo, 26 pp.
[13]Fouquart, Y., and B. Bonnel, 1980: Computation of solar heating of the Earth's atmosphere: A new parameterization. Beitr. Phys. Atmos., 53, 35-62.
[14]Betts, A.K., and Harshvardhan, 1987: Thermodynamic constraint on the cloud liquid water feedback in climate models. J. Geophys. Res., 92, 8483-8485.
[15]Garand, L., 1983: Some improvements and complements to the infrared emissivity algorithm including a parameterization of the absorption in the continuum region. J. Atmos. Sci., 40, 230-244.
[16]Garand, L., and J. Mailhot, 1990: The influence of infrared radiation in numerical weather forecasts. Preprints of the Seventh Conference on Atmospheric Radiation, American Meteorological Society, Atlanta, GA, 146-151.
[17]Kuo, H.L., 1974: Further studies of the parameterization of the influence of cumulus convection on large-scale flow. J. Atmos. Sci., 31, 1232-1240.
[18]Anthes, R.A., 1977: A cumulus parameterization scheme utilizing a one-dimensional model. Mon. Wea. Rev., 105, 270-286.
[19]Joseph, D., 1980: Navy 10' global elevation values. National Center for Atmospheric Research notes on the FNWC terrain data set, National Center for Atmospheric Research, Boulder, CO, 3 pp.
[20]Pellerin, G., and R. Benoit, 1987: Champs geophysiques de surface, CMC, NWPM 14 [available from the Canadian Meteorological Centre, Dorval, Quebec].
[21]Deardorff, J.W., 1978: Efficient prediction of ground surface temperature and moisture, with inclusion of a layer of vegetation. J. Geophys. Res., 83, 1889-1903.
[22]Louis, J.-F. (ed.), 1984: ECMWF forecast model physical parameterisation. Research Manual No. 3, European Centre for Medium-Range Weather Forecasts, Reading, England.
[23]Charnock, H., 1955: Wind stress on a water surface. Quart. J. Roy. Meteor. Soc., 81, 639-640.
[24]Louis, J.-F., 1981: ECMWF forecast model documentation manual, Vol. 1. European Centre for Medium-Range Weather Forecasts, Reading, England, A1.21-A1.33.
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Last modified September 14, 1995. For further information, contact:Tom Phillips (phillips@tworks.llnl.gov )
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