On the Inflection Point Instability of a Stratified Ekman Boundary Layer.
Abstract
The neutral Ekman boundary layer is known to be dynamically unstable to infinitesimal perturbations under typical geophysical conditions. This paper discusses this instability to twodimensional, simpleharmonic perturbations, for the stratified Ekman layer.While viscosity and Coriolis forces are generally important in setting up the basic mean profile, the inflection point instability can be investigated in the inviscid, nonrotating system limit. However, the singular nature of the resulting secondorder characteristic equation makes it necessary to solve the nonsingular sixthorder, viscous stratified equation. Since typically occurring Reynolds numbers are much larger than critical, emphasis has been placed on investigating the behavior of maximum growth rates versus stratification for large Re. The appropriate dimensionless parameters are found to be: =(2/Ro Re)^{ 1/2 }, and Ra= gS^{4}/K_{mm}K_{h} [where =(2K/ f)^{ 1/2 }, Re= V_{g}/K_{m}, Ro=V_{g}/f and S=(_{z}+g/ cp)/] for the general case, or and RI=gS/V_{z} for the inviscid case.Unstable stratification shifts maximum growth rates toward a longitudinal orientation and shorter wavelengths from the neutral stratification values of leftward orientation angle, =17°, and wavenumber, =0.5. The local Richardson number at the inflection point is found to he the pertinent parameter for the effects of stratification. This instability is damped completely for values of Ri_{i}>0.25. Unstable stratification tends to support the dynamic instability such that the growth rate for this mode is dominant significantly into the convective instability regime.The instability takes the form of counterrotating circular motions which remain qualitatively similar for a wide range of the basic variables.
 Publication:

Journal of Atmospheric Sciences
 Pub Date:
 July 1972
 DOI:
 10.1175/15200469(1972)029<0850:OTIPIO>2.0.CO;2
 Bibcode:
 1972JAtS...29..850B