Journal Article

Parameterization of Mixed Layer Eddies. Part I: Theory and Diagnosis

Fox-Kemper, Baylor, Hallberg, Robert, Ferrari, Raffaele

2008

Overview

Ageostrophic baroclinic instabilities develop within the surface mixed layer of the ocean at horizontal fronts and efficiently restratify the upper ocean. In this paper a parameterization for the restratification driven by finite-amplitude baroclinic instabilities of the mixed layer is proposed in terms of an overturning streamfunction that tilts isopycnals from the vertical to the horizontal. The streamfunction is proportional to the product of the horizontal density gradient, the mixed layer depth squared, and the inertial period. Hence restratification proceeds faster at strong fronts in deep mixed layers with a weak latitude dependence. In this paper the parameterization is theoretically motivated, confirmed to perform well for a wide range of mixed layer depths, rotation rates, and vertical and horizontal stratifications. It is shown to be superior to alternative extant parameterizations of baroclinic instability for the problem of mixed layer restratification. Two companion papers discuss the numerical implementation and the climate impacts of this parameterization.

• Publisher: American Meteorological Society
• Subject: Boundary layer / Buoyancy / Dynamics of the ocean (upper and deep oceans) / Earth, ocean, space / Eddies / Exact sciences and technology / External geophysics / General circulation models / Geophysics. Techniques, methods, instrumentation and models / Marine / Meteorology / Oceanography / Physics of the oceans / Simulation / Upper ocean