Abstract
We perform a linear stability analysis of a finite-amplitude plane inertial wave (of frequency
$\omega$
in the range
$0\le \omega \le f$
, where
$f$
is the Coriolis frequency) by considering the inviscid evolution of three-dimensional (3-D), small-amplitude, short-wavelength perturbations. Characterizing the base flow plane inertial wave by its non-dimensional amplitude
$A$
and the angle
$\varPhi$
that its wavevector makes with the horizontal axis, the local stability equations are solved over the entire range of perturbation wavevector orientations. At sufficiently small
$A$
, 3-D parametric subharmonic instability (PSI) is the only instability mechanism, with the most unstable perturbation wavevector making an angle close to
$60^{\circ }$
with the inertial wave plane. In addition, the most unstable perturbation is shear-aligned with the inertial wave in the inertial wave plane. Further, at large
$\varPhi$
, i.e.
$\omega \approx f,$
there exists a wide range of perturbation wavevectors whose growth rate is comparable to the maximum growth rate. As
$A$
is increased, theoretical PSI estimates become less relevant in describing the instability characteristics, and the dominant instability transitions to a two-dimensional (2-D) shear-aligned instability, which is shown to be driven by third-order resonance. The transition from 3-D PSI to a 2-D shear-aligned instability is shown to be reasonably captured by two different criteria, one based on the nonlinear time scale in the inertial wave and the other being a Rossby-number-based one.
Publisher
Cambridge University Press (CUP)