Do Submesoscales Affect the Large-Scale Structure of the Upper Ocean? ...

Submesoscale baroclinic instabilities have been shown to restratify the surface mixed layer and to seasonally energize submesoscale turbulence in the upper ocean. But do these instabilities also affect the large-scale circulation and stratification of the upper thermocline? This question is addresse...

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Main Author: Menemenlis, Dimitris
Format: Dataset
Language:unknown
Published: Root 2023
Subjects:
Online Access:https://dx.doi.org/10.48577/jpl.nzb1r0
http://dataverse.jpl.nasa.gov/citation?persistentId=doi:10.48577/jpl.NZB1R0
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spelling ftdatacite:10.48577/jpl.nzb1r0 2024-09-09T19:56:56+00:00 Do Submesoscales Affect the Large-Scale Structure of the Upper Ocean? ... Menemenlis, Dimitris 2023 https://dx.doi.org/10.48577/jpl.nzb1r0 http://dataverse.jpl.nasa.gov/citation?persistentId=doi:10.48577/jpl.NZB1R0 unknown Root dataset Dataset 2023 ftdatacite https://doi.org/10.48577/jpl.nzb1r0 2024-06-17T09:11:51Z Submesoscale baroclinic instabilities have been shown to restratify the surface mixed layer and to seasonally energize submesoscale turbulence in the upper ocean. But do these instabilities also affect the large-scale circulation and stratification of the upper thermocline? This question is addressed for the North Atlantic subtropical mode water region with a series of numerical simulations at varying horizontal grid spacings (16, 8, 4, and 2 km). These simulations are realistically forced and integrated long enough for the thermocline to adjust to the presence or absence of submesoscales. Linear stability analysis indicates that a 2 km grid spacing is sufficient to resolve the most unstable mode of the wintertime mixed-layer instability. As the resolution is increased, spectral slopes of horizontal kinetic energy flatten and vertical velocities increase in magnitude, consistent with previous regional and short-time simulations. The equilibrium stratification of the thermocline changes drastically as the ... Dataset North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language unknown
description Submesoscale baroclinic instabilities have been shown to restratify the surface mixed layer and to seasonally energize submesoscale turbulence in the upper ocean. But do these instabilities also affect the large-scale circulation and stratification of the upper thermocline? This question is addressed for the North Atlantic subtropical mode water region with a series of numerical simulations at varying horizontal grid spacings (16, 8, 4, and 2 km). These simulations are realistically forced and integrated long enough for the thermocline to adjust to the presence or absence of submesoscales. Linear stability analysis indicates that a 2 km grid spacing is sufficient to resolve the most unstable mode of the wintertime mixed-layer instability. As the resolution is increased, spectral slopes of horizontal kinetic energy flatten and vertical velocities increase in magnitude, consistent with previous regional and short-time simulations. The equilibrium stratification of the thermocline changes drastically as the ...
format Dataset
author Menemenlis, Dimitris
spellingShingle Menemenlis, Dimitris
Do Submesoscales Affect the Large-Scale Structure of the Upper Ocean? ...
author_facet Menemenlis, Dimitris
author_sort Menemenlis, Dimitris
title Do Submesoscales Affect the Large-Scale Structure of the Upper Ocean? ...
title_short Do Submesoscales Affect the Large-Scale Structure of the Upper Ocean? ...
title_full Do Submesoscales Affect the Large-Scale Structure of the Upper Ocean? ...
title_fullStr Do Submesoscales Affect the Large-Scale Structure of the Upper Ocean? ...
title_full_unstemmed Do Submesoscales Affect the Large-Scale Structure of the Upper Ocean? ...
title_sort do submesoscales affect the large-scale structure of the upper ocean? ...
publisher Root
publishDate 2023
url https://dx.doi.org/10.48577/jpl.nzb1r0
http://dataverse.jpl.nasa.gov/citation?persistentId=doi:10.48577/jpl.NZB1R0
genre North Atlantic
genre_facet North Atlantic
op_doi https://doi.org/10.48577/jpl.nzb1r0
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