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The influence of submesoscales and vertical mixing on the export of sinking tracers in large-eddy simulations

Accepted version
Peer-reviewed

Type

Article

Change log

Authors

Taylor, JR 
Smith, KM 
Vreugdenhil, CA 

Abstract

jats:titleAbstract</jats:title>jats:pWe use idealized large-eddy simulations (LES) and a simple analytical theory to study the influence of submesoscales on the concentration and export of sinking particles from the mixed layer. We find that restratification of the mixed layer following the development of submesoscales reduces the rate of vertical mixing which, in turn, enhances the export rate associated with gravitational settling. For a neutral tracer initially confined to the mixed layer, subinertial (submesoscale) motions enhance the downward tracer flux, consistent with previous studies. However, the sign of the advective flux associated with the concentration of sinking particles reverses, indicating reentrainment into the mixed layer. A new theory is developed to model the gravitational settling flux when the particle concentration is nonuniform. The theory broadly agrees with the LES results and allows us to extend the analysis to a wider range of parameters.</jats:p>

Description

Keywords

Fronts, Mixing, Small scale processes, Turbulence

Journal Title

Journal of Physical Oceanography

Conference Name

Journal ISSN

0022-3670
1520-0485

Volume Title

50

Publisher

American Meteorological Society

Rights

All rights reserved