Some Remarks on the Treatment of Finite Amplitude Disturbances in the Baroclinic Atmosphere

K. Gambo
1966 Journal of the Meteorological Society of Japan  
By making use of a two-level, quasi-geostrophic model without friction or heat sources, Corresponding to (2.11) , the quasi-geostrophic vorticity equations at the levels 1 and 3 may be written * In the following discussion , the superscript and prime is omitted for the sake of convenience.
doi:10.2151/jmsj1965.44.2_109 fatcat:st7ch3llwjdytewaybusdrdxae