Summary
Relaxation coefficients for Davies' lateral boundary scheme for limited-area numerical weather prediction models are constructed in such a way that, under idealized conditions, the unwanted partial reflection of outgoing waves (leaving the limited area) at the boundary is minimized.
Similar content being viewed by others
References
Davies, H. C., 1976: A lateral boundary formulation for multi-level prediction models.Quart. J. Roy. Meteor. Soc.,102, 405–418.
Davies, H. C., 1983: Limitations of some common lateral boundary schemes used in regional NWP models.Mon. Wea. Rev.,111, 1002–1012.
Fletcher, R., 1971: A general quadratic programming algorithm.J. Inst. Math. Appl.,7, 1–20.
Giorgi, F., 1990: Simulation of regional climate using a limited area model nested in a general circulation model.J. Climate,3, 941–963.
Kållberg, P., 1977: Test of a lateral boundary relaxation scheme in a barotropic model. ECMWF, Research Department, Internal Report 3, Bracknell.
Pšeničnyj, B. N., 1972:Notwendige Optimalitätsbedingungen. Leipzig: B. G. Teubner.
Pshenichny, B. N., Danilin, Y. M., 1978:Numerical Methods in Extremal Problems. Moscow: Mir Publishers.
Author information
Authors and Affiliations
Additional information
With 2 Figures
Rights and permissions
About this article
Cite this article
Lehmann, R. On the choice of relaxation coefficients for Davies' lateral boundary scheme for regional weather prediction models. Meteorl. Atmos. Phys. 52, 1–14 (1993). https://doi.org/10.1007/BF01025749
Received:
Revised:
Issue Date:
DOI: https://doi.org/10.1007/BF01025749