Modulation of eddy kinetic energy, temperature variance, and eddy heat fluxes by surface buoyancy forcing

Although mesoscale eddies are a ubiquitous feature of the world's oceans, mechanisms determining their strength and variability remain poorly understood. Here we investigate the effects of surface buoyancy forcing on eddy kinetic energy (EKE), temperature variance, and lateral eddy heat fluxes....

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Main Authors: Munday, D, Zhai, X
Format: Journal article
Language:English
Published: 2013
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author Munday, D
Zhai, X
author_facet Munday, D
Zhai, X
author_sort Munday, D
collection OXFORD
description Although mesoscale eddies are a ubiquitous feature of the world's oceans, mechanisms determining their strength and variability remain poorly understood. Here we investigate the effects of surface buoyancy forcing on eddy kinetic energy (EKE), temperature variance, and lateral eddy heat fluxes. In keeping with previous investigations, sustained heat loss ultimately leads to an increase in the magnitude of EKE, whereas sustained heat gain only alters the spatial pattern of EKE, albeit enhancing the temperature variance. These changes to the eddy field and stratification are shown to result in changes in meridional eddy heat flux and residual meridional overturning circulation, which acts to bring the system to equilibrium with the applied surface buoyancy forcing. © 2012 Elsevier Ltd.
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spelling oxford-uuid:bc2995ea-2d69-4688-a81c-242fcb7e80102022-03-27T05:22:19ZModulation of eddy kinetic energy, temperature variance, and eddy heat fluxes by surface buoyancy forcingJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:bc2995ea-2d69-4688-a81c-242fcb7e8010EnglishSymplectic Elements at Oxford2013Munday, DZhai, XAlthough mesoscale eddies are a ubiquitous feature of the world's oceans, mechanisms determining their strength and variability remain poorly understood. Here we investigate the effects of surface buoyancy forcing on eddy kinetic energy (EKE), temperature variance, and lateral eddy heat fluxes. In keeping with previous investigations, sustained heat loss ultimately leads to an increase in the magnitude of EKE, whereas sustained heat gain only alters the spatial pattern of EKE, albeit enhancing the temperature variance. These changes to the eddy field and stratification are shown to result in changes in meridional eddy heat flux and residual meridional overturning circulation, which acts to bring the system to equilibrium with the applied surface buoyancy forcing. © 2012 Elsevier Ltd.
spellingShingle Munday, D
Zhai, X
Modulation of eddy kinetic energy, temperature variance, and eddy heat fluxes by surface buoyancy forcing
title Modulation of eddy kinetic energy, temperature variance, and eddy heat fluxes by surface buoyancy forcing
title_full Modulation of eddy kinetic energy, temperature variance, and eddy heat fluxes by surface buoyancy forcing
title_fullStr Modulation of eddy kinetic energy, temperature variance, and eddy heat fluxes by surface buoyancy forcing
title_full_unstemmed Modulation of eddy kinetic energy, temperature variance, and eddy heat fluxes by surface buoyancy forcing
title_short Modulation of eddy kinetic energy, temperature variance, and eddy heat fluxes by surface buoyancy forcing
title_sort modulation of eddy kinetic energy temperature variance and eddy heat fluxes by surface buoyancy forcing
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AT zhaix modulationofeddykineticenergytemperaturevarianceandeddyheatfluxesbysurfacebuoyancyforcing