Surface Quasigeostrophic Turbulence in Variable Stratification

TL;DR

This paper extends surface quasigeostrophic theory to variable stratification, explaining how stratification affects surface turbulence spectra and providing a method to infer stratification from satellite data.

Contribution

The authors generalize surface quasigeostrophic theory to account for variable stratification, revealing its impact on surface buoyancy anomalies and turbulence spectra.

Findings

Surface buoyancy anomalies influence velocity fields depending on stratification.

Steeper kinetic energy spectra occur over decreasing stratification.

Predicted spectra align with observed wintertime North Atlantic data.

Abstract

Numerical and observational evidence indicates that, in regions where mixed-layer instability is active, the surface geostrophic velocity is largely induced by surface buoyancy anomalies. Yet, in these regions, the observed surface kinetic energy spectrum is steeper than predicted by uniformly stratified surface quasigeostrophic theory. By generalizing surface quasigeostrophic theory to account for variable stratification, we show that surface buoyancy anomalies can generate a variety of dynamical regimes depending on the stratification's vertical structure. Buoyancy anomalies generate longer range velocity fields over decreasing stratification and shorter range velocity fields over increasing stratification. As a result, the surface kinetic energy spectrum is steeper over decreasing stratification than over increasing stratification. An exception occurs if the near surface stratification is much larger than the deep ocean stratification. In this case, we find an extremely local turbulent regime with surface buoyancy homogenization and a steep surface kinetic energy spectrum, similar to equivalent barotropic turbulence. By applying the variable stratification theory to the wintertime North Atlantic, and assuming that mixed-layer instability acts as a narrowband small-scale surface buoyancy forcing, we obtain a predicted surface kinetic energy spectrum between $k^{-4/3}$ and $k^{-7/3}$, which is consistent with the observed wintertime $k^{-2}$ spectrum. We conclude by suggesting a method of measuring the buoyancy frequency's vertical structure using satellite observations.