Abstract
The spurious mass losses or gains due to the anelastic continuity equation are assessed, and the implications of this effect are discussed for the case of the simulation of sea breezes.
Similar content being viewed by others
References
Estoque, M. A.: 1961, ‘A Theoretical Investigation of the Sea Breeze’, Quart. J. Roy. Meteorol. Soc. 87, 136–146.
Huss, A. and Feliks, Y.: 1981, ‘A Mesometeorological Numerical Model of the Sea and Land Breeze, involving Sea Atmospheric Interactions’, Beitr. Phys. Atmos. 54, 238–257.
McPherson, R. D.: 1970, ‘A Numerical Study of the Effect of a Coastal Irregularity on the Sea Breeze’, J. Appl. Meteorol. 7, 767–777.
Neumann, J. and Mahrer, Y.: 1973, ‘Evolution of a Sea Breeze Front: A Numerical Study’, Bonner Meteorologische Abhandlungen 17, 481–492.
Neumann, J. and Mahrer, Y.: 1975, ‘A Theoretical Study of the Lake and Land Breezes of Circular Lakes’, Monthly Weather Rev. 103, 474–485.
Pearce, R.: 1955, ‘The Calculation of the Sea Breeze Circulation in Terms of the Differential Heating Across the Coastline’, Quart. J. Roy. Meteorol. Soc. 81, 351–381.
Pielke, R. A.: 1974, ‘A Three Dimensional Numerical Model of the Sea Breezes over South Florida’, Monthly Weather Rev. 102, 115–139.
Plate, E. J.: 1971, Aerodynamic Characteristics of Atmospheric Boundary Layers, Oak Ridge, Tenn., U. S. Atomic Energy Commission, p. 57.
Wippermann, F.: 1977, ‘Die Grenzen einer Verwendung der hydrostatischen Approximation in mesoskaligen Simulationsmodellen’, Bonnenberg-Drescher, Vorhabensbericht, Nr. 2, 21 p.
Yau, Man Kong: 1980, ‘The Effect of Evaporation, Water Load and Wind Shear on Cloud Development in Three-Dimensional Numerical Models’, J. Atmos. Sci. 37, 488–494.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Feliks, Y., Huss, A. Spurious mass loss in some mesometeorological models. Boundary-Layer Meteorol 24, 387–391 (1982). https://doi.org/10.1007/BF00121602
Revised:
Issue Date:
DOI: https://doi.org/10.1007/BF00121602