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...
Main Authors: | , |
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格式: | Journal article |
語言: | English |
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2007
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_version_ | 1826288493383385088 |
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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 |