Reduced-Order Quasilinear Model of Ocean Boundary-Layer Turbulence

Author:

Skitka Joseph1,Marston J. B.1,Fox-Kemper Baylor2

Affiliation:

1. Department of Physics, Brown University, Providence, Rhode Island

2. Department of Earth, Environmental, and Planetary Science, Brown University, Providence, Rhode Island

Abstract

AbstractThe combined effectiveness of model reduction and the quasilinear approximation for the reproduction of the low-order statistics of oceanic surface boundary layer turbulence is investigated. Idealized horizontally homogeneous problems of surface-forced thermal convection and Langmuir turbulence are studied in detail. Model reduction is achieved with a Galerkin projection of the governing equations onto a subset of modes determined by proper orthogonal decomposition (POD). When applied to boundary layers that are horizontally homogeneous, POD and a horizontally averaged quasilinear approximation both assume flow features that are horizontally wavelike, making the pairing very efficient. For less than 0.2% of the modes retained, the reduced quasilinear model is able to reproduce vertical profiles of horizontal mean fields as well as certain energetically important second-order turbulent transport statistics and energies to within 30% error. Reduced-basis quasilinear statistics must approach the full-basis statistics as the basis size approaches completion; however, some quasilinear statistics resemble those found in the fully nonlinear simulations at smaller basis truncations. Thus, model reduction could possibly improve upon the accuracy of quasilinear dynamics.

Funder

National Science Foundation

Institute at Brown for Environment and Society, Brown University

Publisher

American Meteorological Society

Subject

Oceanography

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