Another look at CISK in polar oceanic air masses.

Some further theoretical results concerning conditional instability of the second kind (CISK) are derived from Bratseth's model and verified for a more general non-Boussinesq model with a z-dependent heating function. In particular, the minimum threshold moisture content required for the instability, is shown to depend only upon environmental stratification and the vertical distribution of latent heat, while the preferred marginally unstable wavelength, in addition to being dependent on the stratification and the heating distribution, is also proportional to the inverse of the Coriolis parameter. A CISK index is used for assessing the relative potential for the CISK development in the Atlantic and the Pacific polar oceanic air masses, compared with that in a tropical oceanic air mass. The limitation arising from use of a constant heating profile in the interpretation of the short wave cut-off is demonstrated. - from Author