Inferring the zonal distribution of measured changes in the meridional overturning circulation

Recently, hydrographic measurements have been used to argue that the meridional overturning circulation at 25°N has decreased by 30% over the last 50 years. Here we show that the most likely interpretation consistent with this approach (i.e., with the dynamic method together with a level-of-no-motio...

全面介紹

書目詳細資料
Main Authors: de Boer, A, Johnson, H
格式: Journal article
語言:English
出版: 2007
_version_ 1826288493383385088
author de Boer, A
Johnson, H
author_facet de Boer, A
Johnson, H
author_sort de Boer, A
collection OXFORD
description Recently, hydrographic measurements have been used to argue that the meridional overturning circulation at 25°N has decreased by 30% over the last 50 years. Here we show that the most likely interpretation consistent with this approach (i.e., with the dynamic method together with a level-of-no-motion assumption and Ekman dynamics) is that any decrease in strength of the deep western boundary current must have been compensated, not by a basin-wide increase in upper layer southward flow, but by changes in the nonlinear region immediately outside of the Florida Straits.
first_indexed 2024-03-07T02:14:32Z
format Journal article
id oxford-uuid:a1c67d9c-f36d-4cd3-bd6d-febed708045f
institution University of Oxford
language English
last_indexed 2024-03-07T02:14:32Z
publishDate 2007
record_format dspace
spelling oxford-uuid:a1c67d9c-f36d-4cd3-bd6d-febed708045f2022-03-27T02:15:33ZInferring the zonal distribution of measured changes in the meridional overturning circulationJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:a1c67d9c-f36d-4cd3-bd6d-febed708045fEnglishSymplectic Elements at Oxford2007de Boer, AJohnson, HRecently, hydrographic measurements have been used to argue that the meridional overturning circulation at 25°N has decreased by 30% over the last 50 years. Here we show that the most likely interpretation consistent with this approach (i.e., with the dynamic method together with a level-of-no-motion assumption and Ekman dynamics) is that any decrease in strength of the deep western boundary current must have been compensated, not by a basin-wide increase in upper layer southward flow, but by changes in the nonlinear region immediately outside of the Florida Straits.
spellingShingle de Boer, A
Johnson, H
Inferring the zonal distribution of measured changes in the meridional overturning circulation
title Inferring the zonal distribution of measured changes in the meridional overturning circulation
title_full Inferring the zonal distribution of measured changes in the meridional overturning circulation
title_fullStr Inferring the zonal distribution of measured changes in the meridional overturning circulation
title_full_unstemmed Inferring the zonal distribution of measured changes in the meridional overturning circulation
title_short Inferring the zonal distribution of measured changes in the meridional overturning circulation
title_sort inferring the zonal distribution of measured changes in the meridional overturning circulation
work_keys_str_mv AT deboera inferringthezonaldistributionofmeasuredchangesinthemeridionaloverturningcirculation
AT johnsonh inferringthezonaldistributionofmeasuredchangesinthemeridionaloverturningcirculation