A Diagnosis of Anisotropic Eddy Diffusion From a High‐Resolution Global Ocean Model

Abstract Oceanic mesoscale eddies are known to diffuse and stir tracers, and the development of skillful eddy closures is aided considerably by the accurate diagnosis of these processes from eddy‐resolving model statistics. In this work a multiple‐tracers inversion method is applied to a global meso...

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Main Authors: Scott D. Bachman, Baylor Fox‐Kemper, Frank O. Bryan
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2020-02-01
Series:Journal of Advances in Modeling Earth Systems
Subjects:
Online Access:https://doi.org/10.1029/2019MS001904
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spelling doaj-5b00f1c011b7459c83990a157810f6af2020-11-25T03:09:21ZengAmerican Geophysical Union (AGU)Journal of Advances in Modeling Earth Systems1942-24662020-02-01122n/an/a10.1029/2019MS001904A Diagnosis of Anisotropic Eddy Diffusion From a High‐Resolution Global Ocean ModelScott D. Bachman0Baylor Fox‐Kemper1Frank O. Bryan2National Center for Atmospheric Research Boulder CO USADepartment of Earth, Environmental, and Planetary Sciences Brown University Providence RI USANational Center for Atmospheric Research Boulder CO USAAbstract Oceanic mesoscale eddies are known to diffuse and stir tracers, and the development of skillful eddy closures is aided considerably by the accurate diagnosis of these processes from eddy‐resolving model statistics. In this work a multiple‐tracers inversion method is applied to a global mesoscale eddy‐resolving simulation, with the intent to solve for the eddy transport tensor that describes the eddy diffusion (symmetric part) and stirring (antisymmetric part). Special emphasis is placed on diagnosing the anisotropy of the horizontal transport, which is described by the eigenvalues and eigenvectors of the 2×2 horizontal symmetric subtensor. Global diagnoses of these quantities, along with an examination of their vertical structures, are used to recommend an algorithm for extending the Gent and McWilliams and Redi parameterizations to include anisotropic effects.https://doi.org/10.1029/2019MS001904mesoscale eddiesGent‐McWilliamseddy diffusionanisotropicsymmetric tensor
collection DOAJ
language English
format Article
sources DOAJ
author Scott D. Bachman
Baylor Fox‐Kemper
Frank O. Bryan
spellingShingle Scott D. Bachman
Baylor Fox‐Kemper
Frank O. Bryan
A Diagnosis of Anisotropic Eddy Diffusion From a High‐Resolution Global Ocean Model
Journal of Advances in Modeling Earth Systems
mesoscale eddies
Gent‐McWilliams
eddy diffusion
anisotropic
symmetric tensor
author_facet Scott D. Bachman
Baylor Fox‐Kemper
Frank O. Bryan
author_sort Scott D. Bachman
title A Diagnosis of Anisotropic Eddy Diffusion From a High‐Resolution Global Ocean Model
title_short A Diagnosis of Anisotropic Eddy Diffusion From a High‐Resolution Global Ocean Model
title_full A Diagnosis of Anisotropic Eddy Diffusion From a High‐Resolution Global Ocean Model
title_fullStr A Diagnosis of Anisotropic Eddy Diffusion From a High‐Resolution Global Ocean Model
title_full_unstemmed A Diagnosis of Anisotropic Eddy Diffusion From a High‐Resolution Global Ocean Model
title_sort diagnosis of anisotropic eddy diffusion from a high‐resolution global ocean model
publisher American Geophysical Union (AGU)
series Journal of Advances in Modeling Earth Systems
issn 1942-2466
publishDate 2020-02-01
description Abstract Oceanic mesoscale eddies are known to diffuse and stir tracers, and the development of skillful eddy closures is aided considerably by the accurate diagnosis of these processes from eddy‐resolving model statistics. In this work a multiple‐tracers inversion method is applied to a global mesoscale eddy‐resolving simulation, with the intent to solve for the eddy transport tensor that describes the eddy diffusion (symmetric part) and stirring (antisymmetric part). Special emphasis is placed on diagnosing the anisotropy of the horizontal transport, which is described by the eigenvalues and eigenvectors of the 2×2 horizontal symmetric subtensor. Global diagnoses of these quantities, along with an examination of their vertical structures, are used to recommend an algorithm for extending the Gent and McWilliams and Redi parameterizations to include anisotropic effects.
topic mesoscale eddies
Gent‐McWilliams
eddy diffusion
anisotropic
symmetric tensor
url https://doi.org/10.1029/2019MS001904
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