Share  Bookmark

 Download from


I p 2 D 2 3n2 4 p 2 D 2 + n z shown as function of L in fig. 3 . Acknowledgement. I whish to express my gratitude to Prof. R. Fjarrtoft for his helpful suggestions.
FJBRTOFT, R., 1950: Application of integral theorems in deriving criteria of stability for laminar flows and for the baroclinic circular vortex. Geof. Publ. 17. 6 , 52 PP.
 1951: Report on work at U.C.L.A. Department of Meteorology under contract (W28099 aC403).
H0ILAND, E., 1952: Perturbation of infinite wavelength of a linear flow with a harmonic velocity profile. VidenskapsAkademiets Instituft for V a r  og Klimaforskning, Rapport nr. a, 3 pp.
Kuo,H.L., 1949: Dynamic instability of twodimensional nondivergent flow in a barotropic atmosphere. J . Meteor. 6, pp. 10s  122.