References
- Arakawa, A. and Lamb, V. R. 1977. Computational design of the basic dynamical process of the UCLA general circulation model. Meth. Comput. Phys. 17, 173–265.
- Baines, P. G. 1995. Topographic effects in startified flows. Cambridge University Press, New York.
- Bubnova, R., Hello, G., Benard, P. and Geleyn, J. F. 1995. Integration of fully elastic equations cast in the hydrostatic pressure terrain-following coordinate in the framework of the ARPEGE/Aladin NWP system. Mon. Wea. Re v. 123, 515–535.
- Carpenter, K. M. 1979. An experimental forecast using a nonhydrostatic mesoscale model. Q. J. R. Meteorol. Soc. 105, 629–655.
- Davies, H. C. 1976. A lateral boundary formulation for multi-level prediction models. Q. J. R. Meteorol. Soc. 102,405–418.
- Dudhia, J. 1993. A nonhydroatatic version of the Penn State-NCAR mesoscale model: validation tests and simulation of an Atlantic cyclone and cold front. Mon. Wea. Re v. 121, 1493–1513.
- Eliassen, A. 1949. The quasi-static equations of motion with pressure as indipendent variable. Geofys. Publ. (Oslo) 17, 1–44.
- Laprise, R. 1992. The Euler equations of motion with hydro-static pressure as an indipendent variable. Mon. Wea. Re v. 120, 197–207.
- Laprise, R. and Peltier, W. R. 1989. On the structural characteristics of steady finite-amplitude mountain waves over bell-shaped topography. J. Atmos. Sc i. 46, 586–595.
- Männilc, A. and Room, R. 2001. Non-hydrostatic adiabatic kernel for HIRLAM. Part II. Anelastic, hybrid-coordinate, explicit-Eulerian model. HIRLAM Technical Report 49, 54 pp. Available from the HIRLAM member institutes or http://www.knmi.n1/hirlamicechReportsila49ab.html.
- Miller, M. 1974. On the use of pressure as vertical coordinate in modeling convection. Q. J. R. Meteorol. Soc. 100, 155–162.
- Miller, M. and Pearce, R. P. 1974. A three-dimensional prim-itive equation model of cumulonimbus convection. Q. J. R. Meteorol. Soc. 100, 133–154.
- Robert, A. 1982. A semi-Lagrangian and semi-implicit numerical scheme for the primitive meteorological equations. J. Meteorol. Soc. Jpn. 60, 319–325.
- Robert, A. J., Henderson, H. and Turnbull, C. 1972. An implicit time integration scheme for baroclinic modes of the atmosphere. Mon. Wea. Re v. 100, 329–335.
- R˜o˜om, R. 2001. Nonhydrostatic adiabatic kernel for HIRLAM. Part I: Fundametals of nonhydrostatic dynamics in pressure-related coordinates. HIRLAM Technical Report 48,26 pp. Available from the HIRLAM member institutes or http://www.knmi.nl/hirlam/TechReports/T’R48ab.html.
- R˜o˜om, R. and Männilc, A. 2002. Non-hydrostatic adiabatic kernel for HIRLAM. Part BI. semi-implicit Eulerian scheme. HIRLAM Technical Report 55, 25 pp. Available from the HIRLAM member institutes or http://www.knmi.nl/hirlamifechReports/TR55ab.html.
- R˜o˜om, R., Miranda, P. and Thorpe, A. 2001. Filtered non-hydrostatic models in pressure related coordinates. Q. J. R. MeteoroL Soc. 127, 1277–1291.
- R˜o˜om, R. 1990. General form of the dynamical equations for the ideal atmosphere in the isobaric coordinate system. Izvestia, Atmos. and Oceanic Phys. 26, 9–14.
- Salmon, R. and Smith, L. M. 1994. Hamiltonian derivation of the nonhydrostatic pressure-coordinate model. Q. J. R. MeteoroL Soc. 120, 1409–1413.
- Simmons, A. J. and Burridge, D. M. 1981. An energy and angular momentum conserving vertical finite difference scheme and hybrid vertical coordinates. Mon. Wea. Rev. 109, 109–766.
- Tanguay, M., Robert, A. and Laprise, R. 1990. A semi-implicit semi-Lagrangian fully compressible regional forecast model. Mon. Wea. Rev. 118, 1970–1980.
- Tripoli, G. J. 1992. A nonhydrostatic meoscale model designed to simulate scale interaction. Mon. Wea. Rev. 120, 120–1359.
- White, A. A. 1989. An extended version of nonhydrostatic, pressure coordinate model. Q. J. R. MeteoroL Soc. 115, 1243–1251.
- Yeh, K.-S., Cote, J.,Gravel, S., Methot, A., Patoine, A., Roch, M. and Staniforth, A. 2002. The CMC-MRB Global Environmental Multiscale (GEM) Model. Part BI: Nonhydrostatic Formulation. Mon. Wea. Rev. 130, 130–356.