Towards measuring the meridional overturning circulation from space

We present a step towards measuring the meridional overturning circulation (MOC), i.e. the full-depth water mass transport, in the North Atlantic using satellite data. Using the Parallel Ocean Climate Model, we simulate satellite observations of ocean bottom pressure and sea surface height (SSH) ove...

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Main Authors: R. Tokmakian, R. E. Houseago-Stokes, P. Challenor, A. G. P. Shaw, D. Cromwell
Format: Article
Language:English
Published: Copernicus Publications 2007-05-01
Series:Ocean Science
Online Access:http://www.ocean-sci.net/3/223/2007/os-3-223-2007.pdf
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author R. Tokmakian
R. E. Houseago-Stokes
P. Challenor
A. G. P. Shaw
D. Cromwell
author_facet R. Tokmakian
R. E. Houseago-Stokes
P. Challenor
A. G. P. Shaw
D. Cromwell
author_sort R. Tokmakian
collection DOAJ
description We present a step towards measuring the meridional overturning circulation (MOC), i.e. the full-depth water mass transport, in the North Atlantic using satellite data. Using the Parallel Ocean Climate Model, we simulate satellite observations of ocean bottom pressure and sea surface height (SSH) over the 20-year period from 1979–1998, and use a linear model to estimate the MOC. As much as 93.5% of the variability in the smoothed transport is thereby explained. This increases to 98% when SSH and bottom pressure are first smoothed. We present initial studies of predicting the time evolution of the MOC, with promising results. It should be stressed that this is an initial step only, and that to produce an actual working system for measuring the MOC from space would require considerable future work.
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spelling doaj.art-7277b42b02334882a2e04a41d748e9252022-12-21T23:15:57ZengCopernicus PublicationsOcean Science1812-07841812-07922007-05-0132223228Towards measuring the meridional overturning circulation from spaceR. TokmakianR. E. Houseago-StokesP. ChallenorA. G. P. ShawD. CromwellWe present a step towards measuring the meridional overturning circulation (MOC), i.e. the full-depth water mass transport, in the North Atlantic using satellite data. Using the Parallel Ocean Climate Model, we simulate satellite observations of ocean bottom pressure and sea surface height (SSH) over the 20-year period from 1979–1998, and use a linear model to estimate the MOC. As much as 93.5% of the variability in the smoothed transport is thereby explained. This increases to 98% when SSH and bottom pressure are first smoothed. We present initial studies of predicting the time evolution of the MOC, with promising results. It should be stressed that this is an initial step only, and that to produce an actual working system for measuring the MOC from space would require considerable future work.http://www.ocean-sci.net/3/223/2007/os-3-223-2007.pdf
spellingShingle R. Tokmakian
R. E. Houseago-Stokes
P. Challenor
A. G. P. Shaw
D. Cromwell
Towards measuring the meridional overturning circulation from space
Ocean Science
title Towards measuring the meridional overturning circulation from space
title_full Towards measuring the meridional overturning circulation from space
title_fullStr Towards measuring the meridional overturning circulation from space
title_full_unstemmed Towards measuring the meridional overturning circulation from space
title_short Towards measuring the meridional overturning circulation from space
title_sort towards measuring the meridional overturning circulation from space
url http://www.ocean-sci.net/3/223/2007/os-3-223-2007.pdf
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AT agpshaw towardsmeasuringthemeridionaloverturningcirculationfromspace
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