A Simple Example of Galilean Invariance in the Omega Equation

Bulletin of the American Meteorological Society

Volumn 82, Issue 3, 2001, Pages 463-472

  Walters, Michael K ^a  

^a AIR FORCE INSTITUTE OF TECHNOLOGY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0043236337     PISSN: 00030007     EISSN: None     Source Type: Journal    
DOI: 10.1175/1520-0477(2001)082<0463:ASEOGI>2.3.CO;2     Document Type: Article

References (10)

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2. Charney, J. G., 1947: The dynamics of long waves in a baroclinic westerly current. J. Meteor., 4, 135-163.
3. Durran, D. R., and L. W. Snellman, 1987: The diagnosis of synoptic-scale vertical motion in an operational environment. Wea. Forecasting, 2, 17-31.
4. Eady, E. T., 1949: Long waves and cyclone waves. Tellus, 1 (3), 33-52.
5. Holton, J. R., 1992: An Introduction to Dynamic Meteorology. Academic Press, 507 pp.
6. Hoskins, B. J., I. Draghici, and H. C. Davies, 1978: A new look at the ω-equation. Quart. J. Roy. Meteor. Soc., 104, 31-38.
7. James, I., 1994: Introduction to Circulating Atmospheres. Cambridge University Press, 422 pp.
8. Morgan, M. C., and J. W. Nielson-Gammon, 1998: Using tropopause maps to diagnose midlatitude weather systems. Mon. Wea. Rev., 126, 2555-2579.
9. Pedlosky, J., 1987: Geophysical Fluid Dynamics. Springer-Verlag, 710 pp.
10. Trenberth, K. E., 1978: On the interpretation of the diagnostic QG omega equation. Mon. Wea. Rev., 106, 131-137.