Reconsideration of Orlanski's instability theory of frontal waves

Abstract

This paper complements the instability theory of frontal waves investigated by Orlanski (1968), and reinterprets the unstable modes obtained. First, the stability of a frontal model is reconsidered by using a matrix method. The major part of Orlanski's (1968) result is verified but some flaws are found in some parameter regions: unstable modes do not exist over the entire Ri–Ro region. Also, the features of the neutral waves in the one-layer subsystems are studied, in order to determine the instability of the full two-layer system. As a result, the unstable mode called the (B)-mode by Orlanski (1968) and suggested by Sakai (1989) to be Rossby-Kelvin instability caused by a resonance between a Rossby wave and a gravity wave, proves to be a geostrophic unstable mode caused by resonance between a Rossby wave and the Rossby-gravity mixed mode. In addition, some of the analytical conclusions about the stability of this frontal model are explained by the features of the neutral waves in the one-layer subsystem.