Forward and inverse kinetic energy cascades in Jupiter’s turbulent weather layer

Jupiter’s turbulent weather layer contains phenomena of many different sizes, from local storms up to the Great Red Spot and banded jets. The global circulation is driven by complex interactions with (as yet uncertain) small scale processes. We have calculated structure functions and kinetic energy...

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Main Authors: Young, R, Read, P
Format: Journal article
Language:English
Published: Nature Publishing Group 2017
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author Young, R
Read, P
author_facet Young, R
Read, P
author_sort Young, R
collection OXFORD
description Jupiter’s turbulent weather layer contains phenomena of many different sizes, from local storms up to the Great Red Spot and banded jets. The global circulation is driven by complex interactions with (as yet uncertain) small scale processes. We have calculated structure functions and kinetic energy spectral fluxes from Cassini observations over a wide range of length scales in Jupiter’s atmosphere. We found evidence for an inverse cascade of kinetic energy from length scales comparable with the first baroclinic Rossby deformation radius to the global jet scale, but also a forward cascade of kinetic energy from the deformation radius to smaller scales. The latter disagrees with the traditional picture of Jupiter’s atmospheric dynamics, but has some similarities with mesoscale phenomena in the Earth’s atmosphere and oceans. We conclude that the inverse cascade driving Jupiter’s jets may have a dominant energy source at scales close to the deformation radius, such as baroclinic instability.
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spelling oxford-uuid:9e8db436-e990-49e7-b1af-2b6182d9fb032022-03-27T00:50:57ZForward and inverse kinetic energy cascades in Jupiter’s turbulent weather layerJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:9e8db436-e990-49e7-b1af-2b6182d9fb03EnglishSymplectic Elements at OxfordNature Publishing Group2017Young, RRead, PJupiter’s turbulent weather layer contains phenomena of many different sizes, from local storms up to the Great Red Spot and banded jets. The global circulation is driven by complex interactions with (as yet uncertain) small scale processes. We have calculated structure functions and kinetic energy spectral fluxes from Cassini observations over a wide range of length scales in Jupiter’s atmosphere. We found evidence for an inverse cascade of kinetic energy from length scales comparable with the first baroclinic Rossby deformation radius to the global jet scale, but also a forward cascade of kinetic energy from the deformation radius to smaller scales. The latter disagrees with the traditional picture of Jupiter’s atmospheric dynamics, but has some similarities with mesoscale phenomena in the Earth’s atmosphere and oceans. We conclude that the inverse cascade driving Jupiter’s jets may have a dominant energy source at scales close to the deformation radius, such as baroclinic instability.
spellingShingle Young, R
Read, P
Forward and inverse kinetic energy cascades in Jupiter’s turbulent weather layer
title Forward and inverse kinetic energy cascades in Jupiter’s turbulent weather layer
title_full Forward and inverse kinetic energy cascades in Jupiter’s turbulent weather layer
title_fullStr Forward and inverse kinetic energy cascades in Jupiter’s turbulent weather layer
title_full_unstemmed Forward and inverse kinetic energy cascades in Jupiter’s turbulent weather layer
title_short Forward and inverse kinetic energy cascades in Jupiter’s turbulent weather layer
title_sort forward and inverse kinetic energy cascades in jupiter s turbulent weather layer
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