Understanding the regional variability of eddy diffusivity in the Pacific sector of the Southern Ocean

A diagnostic framework is presented, based on the Nakamura effective diffusivity, to investigate the regional variation in eddy diffusivity. Comparison of three different diffusivity calculations enables the effects of locally enhanced tracer diffusion to be distinguished from the streamwise average...

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Published in:Journal of Physical Oceanography
Main Authors: Shuckburgh, Emily, Jones, Helen, Marshall, John, Hill, Chris
Format: Article in Journal/Newspaper
Language:unknown
Published: American Meteorological Society 2009
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/11276/
https://doi.org/10.1175/2009JPO4115.1
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spelling ftnerc:oai:nora.nerc.ac.uk:11276 2023-05-15T18:24:45+02:00 Understanding the regional variability of eddy diffusivity in the Pacific sector of the Southern Ocean Shuckburgh, Emily Jones, Helen Marshall, John Hill, Chris 2009 http://nora.nerc.ac.uk/id/eprint/11276/ https://doi.org/10.1175/2009JPO4115.1 unknown American Meteorological Society Shuckburgh, Emily orcid:0000-0001-9206-3444 Jones, Helen; Marshall, John; Hill, Chris. 2009 Understanding the regional variability of eddy diffusivity in the Pacific sector of the Southern Ocean. Journal of Physical Oceanography, 39 (9). 2011-2023. https://doi.org/10.1175/2009JPO4115.1 <https://doi.org/10.1175/2009JPO4115.1> Marine Sciences Hydrology Publication - Article PeerReviewed 2009 ftnerc https://doi.org/10.1175/2009JPO4115.1 2023-02-04T19:27:17Z A diagnostic framework is presented, based on the Nakamura effective diffusivity, to investigate the regional variation in eddy diffusivity. Comparison of three different diffusivity calculations enables the effects of locally enhanced tracer diffusion to be distinguished from the streamwise average. It also enables the distinction to be made between locally generated complexity in the tracer structure and that advected into a particular domain. The technique is applied to the Pacific sector of the Southern Ocean. The results highlight the important role that the mean flow plays in determining eddy diffusivity. The effective diffusivity is not simply related to the eddy kinetic energy: in regions of a strong mean flow the eddy diffusivity can be suppressed even in the presence of moderately strong eddy activity; conversely, in a region of weak mean flow the eddy diffusivity can be enhanced even in the presence of only weak eddy activity. This casts doubt on the ability of parameterizations based solely on the eddy kinetic energy to adequately characterize the eddy diffusivity in regions of strongly varying mean flow such as the Southern Ocean. The results are, however, consistent with the eddy transport and mixing variability predicted by potential-vorticity-based arguments. Article in Journal/Newspaper Southern Ocean Natural Environment Research Council: NERC Open Research Archive Pacific Southern Ocean Journal of Physical Oceanography 39 9 2011 2023
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
topic Marine Sciences
Hydrology
spellingShingle Marine Sciences
Hydrology
Shuckburgh, Emily
Jones, Helen
Marshall, John
Hill, Chris
Understanding the regional variability of eddy diffusivity in the Pacific sector of the Southern Ocean
topic_facet Marine Sciences
Hydrology
description A diagnostic framework is presented, based on the Nakamura effective diffusivity, to investigate the regional variation in eddy diffusivity. Comparison of three different diffusivity calculations enables the effects of locally enhanced tracer diffusion to be distinguished from the streamwise average. It also enables the distinction to be made between locally generated complexity in the tracer structure and that advected into a particular domain. The technique is applied to the Pacific sector of the Southern Ocean. The results highlight the important role that the mean flow plays in determining eddy diffusivity. The effective diffusivity is not simply related to the eddy kinetic energy: in regions of a strong mean flow the eddy diffusivity can be suppressed even in the presence of moderately strong eddy activity; conversely, in a region of weak mean flow the eddy diffusivity can be enhanced even in the presence of only weak eddy activity. This casts doubt on the ability of parameterizations based solely on the eddy kinetic energy to adequately characterize the eddy diffusivity in regions of strongly varying mean flow such as the Southern Ocean. The results are, however, consistent with the eddy transport and mixing variability predicted by potential-vorticity-based arguments.
format Article in Journal/Newspaper
author Shuckburgh, Emily
Jones, Helen
Marshall, John
Hill, Chris
author_facet Shuckburgh, Emily
Jones, Helen
Marshall, John
Hill, Chris
author_sort Shuckburgh, Emily
title Understanding the regional variability of eddy diffusivity in the Pacific sector of the Southern Ocean
title_short Understanding the regional variability of eddy diffusivity in the Pacific sector of the Southern Ocean
title_full Understanding the regional variability of eddy diffusivity in the Pacific sector of the Southern Ocean
title_fullStr Understanding the regional variability of eddy diffusivity in the Pacific sector of the Southern Ocean
title_full_unstemmed Understanding the regional variability of eddy diffusivity in the Pacific sector of the Southern Ocean
title_sort understanding the regional variability of eddy diffusivity in the pacific sector of the southern ocean
publisher American Meteorological Society
publishDate 2009
url http://nora.nerc.ac.uk/id/eprint/11276/
https://doi.org/10.1175/2009JPO4115.1
geographic Pacific
Southern Ocean
geographic_facet Pacific
Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_relation Shuckburgh, Emily orcid:0000-0001-9206-3444
Jones, Helen; Marshall, John; Hill, Chris. 2009 Understanding the regional variability of eddy diffusivity in the Pacific sector of the Southern Ocean. Journal of Physical Oceanography, 39 (9). 2011-2023. https://doi.org/10.1175/2009JPO4115.1 <https://doi.org/10.1175/2009JPO4115.1>
op_doi https://doi.org/10.1175/2009JPO4115.1
container_title Journal of Physical Oceanography
container_volume 39
container_issue 9
container_start_page 2011
op_container_end_page 2023
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