GEM4 dynamics : Différence entre versions
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*Caya, A., R. Laprise and P. Zwack, 1998: [http://journals.ametsoc.org/doi/pdf/10.1175/1520-0493%281998%29126%3C1707%3ACOUTSM%3E2.0.CO%3B2 '''Consequences of using process splitting for implementing physical forcings in a semi-implicit semi-Lagrangian model.'''] Mon. Wea. Rev. 126(6), 1707-1713. | *Caya, A., R. Laprise and P. Zwack, 1998: [http://journals.ametsoc.org/doi/pdf/10.1175/1520-0493%281998%29126%3C1707%3ACOUTSM%3E2.0.CO%3B2 '''Consequences of using process splitting for implementing physical forcings in a semi-implicit semi-Lagrangian model.'''] Mon. Wea. Rev. 126(6), 1707-1713. | ||
| − | *Girard, C., A. Plante, M. Desgagné, R. McTaggart-Cowan, J. Côté, M. Charron, S. Gravel, V. Lee, A. Patoine, A. Qaddouri, M. Roch, L. Spacek, M. Tanguay, P. A. Vaillancourt and A. Zadra, 2014: Staggered Vertical Discretization of the Canadian Environmental Multiscale (GEM) Model Using a Coordinate of the Log-Hydrostatic-Pressure Type. Mon. Wea. Rev., 142, 1183–1196. | + | *Girard, C., A. Plante, M. Desgagné, R. McTaggart-Cowan, J. Côté, M. Charron, S. Gravel, V. Lee, A. Patoine, A. Qaddouri, M. Roch, L. Spacek, M. Tanguay, P. A. Vaillancourt and A. Zadra, 2014: [http://dx.doi.org/10.1175/MWR-D-13-00255.1 '''Staggered Vertical Discretization of the Canadian Environmental Multiscale (GEM) Model Using a Coordinate of the Log-Hydrostatic-Pressure Type.'''] Mon. Wea. Rev., 142, 1183–1196. |
| − | *Girard, C., and A. Plante, 2013: GEM4.2: A non-hydrostatic atmospheric model (Euler equations) in terrain-following vertical coordinate of the log-hydrostatic-pressure type vertically discretized on a Charney-Phillips grid with simple differences and means, Revision 2. Notes internes. Recherches en prévision numérique, Environment Canada, 59 pp. La version 2011 “GEM4.1 - Revision 1” du document est disponible au site | + | *Girard, C., and A. Plante, 2013: [http://collaboration.cmc.ec.gc.ca/science/rpn/publications/pdf/GEM4.1.pdf '''GEM4.2: A non-hydrostatic atmospheric model (Euler equations) in terrain-following vertical coordinate of the log-hydrostatic-pressure type vertically discretized on a Charney-Phillips grid with simple differences and means, Revision 2. Notes internes.''' Recherches en prévision numérique, Environment Canada, 59 pp. La version 2011 “GEM4.1 - Revision 1” du document est disponible au site (accédé le 4 février 2015) |
| − | (accédé le 4 février 2015) | ||
| − | *Kasahara, A., 1974: | + | *Kasahara, A., 1974: [http://www.atmo.arizona.edu/students/courselinks/spring12/atmo558/Lectures/Vertical%20coordinate%20system.pdf '''Various vertical coordinate systems used for numerical weather prediction.''' Mon. Wea. Rev. 102, 509-522. See also corrigendum: Mon. Wea. Rev. 103, 664. |
| − | http://www.atmo.arizona.edu/students/courselinks/spring12/atmo558/Lectures/Vertical%20coordinate%20system.pdf | ||
| − | See also corrigendum: Mon. Wea. Rev. 103, 664. | ||
| − | *Laprise, R., 1992: | + | *Laprise, R., 1992: [http://journals.ametsoc.org/doi/pdf/10.1175/1520-0493(1992)120%3C0197%3ATEEOMW%3E2.0.CO%3B2 '''The Euler equation of motion with hydrostatic pressure as independent coordinate.''' Mon. Wea. Rev. 120(1), 197-207. |
| − | http://journals.ametsoc.org/doi/pdf/10.1175/1520-0493(1992)120%3C0197%3ATEEOMW%3E2.0.CO%3B2 | ||
| − | *Rivest, C., A. Staniforth, and A. Robert, 1994: | + | *Rivest, C., A. Staniforth, and A. Robert, 1994: [http://journals.ametsoc.org/doi/pdf/10.1175/1520-0493%281994%29122%3C0366%3ASRROSL%3E2.0.CO%3B2 '''Spurious resonant response of semi-Lagrangian discretizations to orographic forcing: Diagnosis and solution.''' Mon. Wea. Rev., 122, 366–376. |
| − | http://journals.ametsoc.org/doi/pdf/10.1175/1520-0493%281994%29122%3C0366%3ASRROSL%3E2.0.CO%3B2 | ||
| − | *Yeh, K.-S., J. Côté, S. Gravel, A. Méthot, A. Patoine, M. Roch and A. Staniforth, 2002: | + | *Yeh, K.-S., J. Côté, S. Gravel, A. Méthot, A. Patoine, M. Roch and A. Staniforth, 2002: [http://journals.ametsoc.org/doi/full/10.1175/1520-0493(2002)130%3C0339:TCMGEM%3E2.0.CO%3B2 '''The CMCMRB Global Environmental Multiscale (GEM) Model. Part III: Nonhydrostatic Formulation.''' Mon. Wea. Rev., 130, 339356. |
| − | http://journals.ametsoc.org/doi/full/10.1175/1520-0493(2002)130%3C0339:TCMGEM%3E2.0.CO%3B2 | ||
=== Other references === | === Other references === | ||
Version depuis le 26 de mai 2015 à 20:17
Matières
Documentation
GEM4: C. Girard & A. Plante (RPN/CMC)
- C. Girard, A. Plante et al. (2013): Staggered Vertical Discretization of the Canadian Environmental Multiscale (GEM) Model Using a Coordinate of the Log-Hydrostatic-Pressure Type
- C. Girard, A. Plante et al. (2011): GEM4.1: A non-hydrostatic atmospheric model (Euler equations)
- C. Girard, A. Plante et al. (2011): GEM4.2: A non-hydrostatic atmospheric model (Euler equations)
- C. Girard, A. Plante et al.: Options for Semi-Lagrangian Trajectory Calculations
GEM4: R. Laprise (UQAM)
- R. Laprise (2015): Formulation dynamique de GEM4
Section 1 : Les équations continues
Section 1 : Les équations continues Annexes
Section 2 : Les équations discrètes à la verticale et dans le temps
Section 2 : Les équations discrètes à la verticale et dans le temps Annexes
Références
- Caya, A., R. Laprise and P. Zwack, 1998: Consequences of using process splitting for implementing physical forcings in a semi-implicit semi-Lagrangian model. Mon. Wea. Rev. 126(6), 1707-1713.
- Girard, C., A. Plante, M. Desgagné, R. McTaggart-Cowan, J. Côté, M. Charron, S. Gravel, V. Lee, A. Patoine, A. Qaddouri, M. Roch, L. Spacek, M. Tanguay, P. A. Vaillancourt and A. Zadra, 2014: Staggered Vertical Discretization of the Canadian Environmental Multiscale (GEM) Model Using a Coordinate of the Log-Hydrostatic-Pressure Type. Mon. Wea. Rev., 142, 1183–1196.
- Girard, C., and A. Plante, 2013: [http://collaboration.cmc.ec.gc.ca/science/rpn/publications/pdf/GEM4.1.pdf GEM4.2: A non-hydrostatic atmospheric model (Euler equations) in terrain-following vertical coordinate of the log-hydrostatic-pressure type vertically discretized on a Charney-Phillips grid with simple differences and means, Revision 2. Notes internes. Recherches en prévision numérique, Environment Canada, 59 pp. La version 2011 “GEM4.1 - Revision 1” du document est disponible au site (accédé le 4 février 2015)
- Kasahara, A., 1974: [http://www.atmo.arizona.edu/students/courselinks/spring12/atmo558/Lectures/Vertical%20coordinate%20system.pdf Various vertical coordinate systems used for numerical weather prediction. Mon. Wea. Rev. 102, 509-522. See also corrigendum: Mon. Wea. Rev. 103, 664.
- Laprise, R., 1992: [http://journals.ametsoc.org/doi/pdf/10.1175/1520-0493(1992)120%3C0197%3ATEEOMW%3E2.0.CO%3B2 The Euler equation of motion with hydrostatic pressure as independent coordinate. Mon. Wea. Rev. 120(1), 197-207.
- Rivest, C., A. Staniforth, and A. Robert, 1994: [http://journals.ametsoc.org/doi/pdf/10.1175/1520-0493%281994%29122%3C0366%3ASRROSL%3E2.0.CO%3B2 Spurious resonant response of semi-Lagrangian discretizations to orographic forcing: Diagnosis and solution. Mon. Wea. Rev., 122, 366–376.
- Yeh, K.-S., J. Côté, S. Gravel, A. Méthot, A. Patoine, M. Roch and A. Staniforth, 2002: [http://journals.ametsoc.org/doi/full/10.1175/1520-0493(2002)130%3C0339:TCMGEM%3E2.0.CO%3B2 The CMCMRB Global Environmental Multiscale (GEM) Model. Part III: Nonhydrostatic Formulation. Mon. Wea. Rev., 130, 339356.
