Non-hydrostatic semi-elastic hybrid-coordinate SISL extension of HIRLAM. Part II: numerical testing
By: Rein Rõõm, Aarne Männik, Andres Luhamaa and Marko Zirk
References
-
Asselin
, R. A.. Frequency filter for time integrations.. 100, 487– 490. -
Baines
, P. G.. Topographic Effects in Stratified Flows. Cambridge Univ. Press, 482 pp. -
Benard
, P.. Stability of semi-implicit and iterative centered-implicit time discretization for various equation systems used in NWP.. 131, 2479– 2491. -
Benard
, P.. On the use of a wider class of linear systems for the design of constant-coefficient semi-implicit time schemes in NWP.. 132, 1319– 1324. -
Bouttier
, F.. Non-hydrostatic dynamical core intercomparisons, Workshop report of HIRLAM Workshop on Mesoscale Modelling, Dublin 14-16 October 2002,52-60, Available from HIRLAM member institutes or http://hirlam. org/open/publicationsalLworkshops/mesoscaleDublinOct 02 -
Bubnova
, R., Hello, G., Bernard, P.and Geleyn, J.-F.. Integration of the fully elastic equations cast in the hydrostatic pressure terrain-following coordinate in the framework of APREGE/Aladin NWP system.. 123, 515– 535. -
Davies
, H. C.. A lateral boundary formulation for multilevel prediction models. Q. J. R. Meteorol. Soc. 102, 405– 418. -
Girard
, C., Benoit, R.and Desgagne, M.. Finescale topography and the MC2 dynamics kernel.. 133, 1463– 1477. -
Ikawa
, M.and Saito, K.. Description of a nonhydrostatic model developed at the Forecast Research Department of the MRI. Technical Reports of the MRI, 28, 238 pp. -
Klemp
, J. B., Skamarock, W. C.and Fuhrer, O.. Numerical consistency of metric terms in terrain-following coordinates.. 131, 1229– 1239. -
Laprise
, R.,. The Euler equations of motion with hydrostatic pressure as an independent variable.. 120, 197– 207. -
Laprise
and Peltier, W. R.. On the structural characteristics of steady finite-amplitude mountain waves over bell-shaped topography.. 46, 586– 595. -
Männilc
, A.. Implementation and validation of the nonhydro-static adiabatic core of the numerical weather prediction model HIRLAM. Dissertationes Geophysicales Universitatis Tartuensis, pp. 88. -
Männilc
, A.and Room, R.. Non-hydrostatic adiabatic kernel for HIRLAM. PartAnelastic, hybrid-coordinate, explicit-Eulerian model. HIRLAIVI Technical Report, 49, p. 54 Available from the HIRLAM member institutes or http://hirlam.org/open/publications/TechReports/T’R49ab.html -
Männilc
, A., Room, R.and Luhamaa, A.. Nonhydrostatic generalization of a pressure-coordinate-based hydrostatic model with implementation in HIRLAM: validation of adiabatic core. Tellus, 219– 231. -
McDonald
, A.. An examination of alternative extrapolations to find the departure point position in a ‘two-time-level’ semi-Lagrangian integration.. 127, 1985– 1993. -
McDonald
and Haugen, J.-E.. A two-time-level, three-dimensional, semi-Lagrangian, semi-implicit, limited-area gridpoint model of the primitive equations. Part Extension to hybrid vertical coordinates.. 121, 2077– 2087. -
Miller
, M. J.. On the use of pressure as vertical co-ordinate in modelling convection. Q. J. R. MeteoroL Soc. 100, 155– 162. -
Miller
, M. J.and Pearce, R. P.. A three-dimensional primitive equation model of cumulonimbus convection. Q. J. R. MeteoroL Soc. 100, 133– 154. -
Miller
, M. J.and White, A. A.. On the nonhydrostatic equations in pressure and sigma coordinates. Q. J. R. MeteoroL Soc. 110, 515– 533. -
Nance
, L. B.and Durran, D.. A modelling study of nonstationary trapped lee waves. Part II: Nonlinearity.. 55, 1429– 1445. -
Pinty
, J.-P., Benoit, R., Richard, E.and Laprise, R.. Simple tests of a semi-implicit semi-Lagrangian model on 2D mountain wave problems.. 123, 3042– 3058. -
Ritchie
, H., Temperton, C., Simmons, A., Hortal, M., Davies, T., and co-authors.. Implementation of the Semi-Lagrangian method in a high-resolution version of the ECMWF forecast model. Mon. Wea. Rev. 123, 489- 514. -
Richie
, H.and Tanguay, M.. A comparison of spatially averaged Eulerian and Lagrangian treatments of mountains.. 124, 167– 181. -
Robert
, A.. The integration of a spectral model of the atmosphere by the implicit method. Proc. WMO/IUGG Symposium on NWP, Japan Meteorological Society, Tolcio, Japan, 19- 24. -
Room
, R.and Männilc, A.. Response of different nonhydrostatic, pressure-coordinate models to orographic forcing.. 56, 2553– 2570. -
Room
, R., Männilc, A.and Luhamaa, A.. Non-hydrostatic, semi-Lagrangian , semi-implicit adiabatic kernel for HIRLAM. Part I: numerical scheme. Tellus, in press. -
Room
, R.and Zirk, M.. Amplitude factorization method in the atmospheric gravitywave equation. Communications in Computational Physics. 2, 993– 1006. -
Schär
, C., Leuenberger, D., Furher, O., Liithi, D.and Girard, C.. A new terrain-following vertical coordinate formulation for atmospheric prediction models.. 130– 2480. -
Shuns
, G.and Broad, A.. A case study of lee waves over the Lake District in northern England. Q. J. R. Meteord. Soc. 119, 377– 409. -
Simmons
, A. J., Hoskins, B. J.and Burridge, D. M.. Stability of the semi—implicit method of time integration.. 106, 405– 412. -
Tanguay
, M., Robert, A.and Laprise, R.. A semi—implicit semi—Lagrangian fully compressible regional model.. 118, 1970– 1980. -
Unden
, P., Rontu, L., Järvinen, H., Lynch, P., Calvo, J., and co-authors. 2002. HIRLAM-5 Scientific Documentation, HIRLAIVI-5 Project, do Per Undén SMHI, S-60I 76 Norrkoping, SWEDEN, 144 p.Available from the HIRLAM member institutes or http://hirlam.org/open/publications/SciDoc_Dec2002.pdf -
White
, A. A.. An extended version of nonhydrostatic, pres-sure coordinate model. Q. J. R. MeteoroL Soc. 115, 1243– 1251.
DOI: https://doi.org/10.1111/j.1600-0870.2007.00253.x | Journal eISSN: 3035-9554
Language: English
Page range: 661 - 673
Submitted on: Aug 9, 2006
Accepted on: Mar 19, 2006
Published on: Jan 1, 2007
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 2007 Rein Rõõm, Aarne Männik, Andres Luhamaa, Marko Zirk, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.