Relative strength of the Antarctic Circumpolar Current and Atlantic Meridional Overturning Circulation

A simple relationship, based on thermal wind balance, is derived that relates the relative strength of the Antarctic Circumpolar Current (ACC) and Atlantic Meridional Overturning Circulation (AMOC) to the ratios of three depth scales: the e-folding depth of the global stratification, the depth of ma...

Full description

Bibliographic Details
Main Authors: David P. Marshall, Helen L. Johnson
Format: Article
Language:English
Published: Stockholm University Press 2017-01-01
Series:Tellus: Series A, Dynamic Meteorology and Oceanography
Subjects:
Online Access:http://dx.doi.org/10.1080/16000870.2017.1338884
_version_ 1818040159976816640
author David P. Marshall
Helen L. Johnson
author_facet David P. Marshall
Helen L. Johnson
author_sort David P. Marshall
collection DOAJ
description A simple relationship, based on thermal wind balance, is derived that relates the relative strength of the Antarctic Circumpolar Current (ACC) and Atlantic Meridional Overturning Circulation (AMOC) to the ratios of three depth scales: the e-folding depth of the global stratification, the depth of maximum overturning streamfunction and the maximum depth of the ACC. For realistic values of these depth scales, the relationship predicts a factor $ 8 \pm 4 $ difference in the volume transports of the ACC and AMOC, consistent with the observation-based ratio of $ 8 \pm 2 $.
first_indexed 2024-12-10T08:10:06Z
format Article
id doaj.art-5ccffabbde6f4d29b6c6390e51c4ed6e
institution Directory Open Access Journal
issn 1600-0870
language English
last_indexed 2024-12-10T08:10:06Z
publishDate 2017-01-01
publisher Stockholm University Press
record_format Article
series Tellus: Series A, Dynamic Meteorology and Oceanography
spelling doaj.art-5ccffabbde6f4d29b6c6390e51c4ed6e2022-12-22T01:56:35ZengStockholm University PressTellus: Series A, Dynamic Meteorology and Oceanography1600-08702017-01-0169110.1080/16000870.2017.13388841338884Relative strength of the Antarctic Circumpolar Current and Atlantic Meridional Overturning CirculationDavid P. Marshall0Helen L. Johnson1University of OxfordUniversity of OxfordA simple relationship, based on thermal wind balance, is derived that relates the relative strength of the Antarctic Circumpolar Current (ACC) and Atlantic Meridional Overturning Circulation (AMOC) to the ratios of three depth scales: the e-folding depth of the global stratification, the depth of maximum overturning streamfunction and the maximum depth of the ACC. For realistic values of these depth scales, the relationship predicts a factor $ 8 \pm 4 $ difference in the volume transports of the ACC and AMOC, consistent with the observation-based ratio of $ 8 \pm 2 $.http://dx.doi.org/10.1080/16000870.2017.1338884ocean currentsvolume transportshydrographythermal windmeridional boundaries
spellingShingle David P. Marshall
Helen L. Johnson
Relative strength of the Antarctic Circumpolar Current and Atlantic Meridional Overturning Circulation
Tellus: Series A, Dynamic Meteorology and Oceanography
ocean currents
volume transports
hydrography
thermal wind
meridional boundaries
title Relative strength of the Antarctic Circumpolar Current and Atlantic Meridional Overturning Circulation
title_full Relative strength of the Antarctic Circumpolar Current and Atlantic Meridional Overturning Circulation
title_fullStr Relative strength of the Antarctic Circumpolar Current and Atlantic Meridional Overturning Circulation
title_full_unstemmed Relative strength of the Antarctic Circumpolar Current and Atlantic Meridional Overturning Circulation
title_short Relative strength of the Antarctic Circumpolar Current and Atlantic Meridional Overturning Circulation
title_sort relative strength of the antarctic circumpolar current and atlantic meridional overturning circulation
topic ocean currents
volume transports
hydrography
thermal wind
meridional boundaries
url http://dx.doi.org/10.1080/16000870.2017.1338884
work_keys_str_mv AT davidpmarshall relativestrengthoftheantarcticcircumpolarcurrentandatlanticmeridionaloverturningcirculation
AT helenljohnson relativestrengthoftheantarcticcircumpolarcurrentandatlanticmeridionaloverturningcirculation