Observed Basin-Scale Response of the North Atlantic Meridional Overturning Circulation to Wind Stress Forcing

<jats:title>Abstract</jats:title> <jats:p>The response of the North Atlantic meridional overturning circulation (MOC) to wind stress forcing is investigated from an observational standpoint, using four time series of overturning transports below and relative to 1000 m, overlapping...

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Published in:Journal of Climate
Main Authors: Elipot, Shane, Frajka-Williams, Eleanor, Hughes, Chris W, Olhede, Sofia, Lankhorst, Matthias
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2017
Subjects:
Online Access:https://livrepository.liverpool.ac.uk/3005780/
https://doi.org/10.1175/jcli-d-16-0664.1
https://livrepository.liverpool.ac.uk/3005780/1/Elipot_et_al_JClim_2017_accepted2016.pdf
https://livrepository.liverpool.ac.uk/3005780/2/2017-Elipot_et_al_JClim_MOC_Basin_Scale_wind.pdf
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spelling ftunivliverpool:oai:livrepository.liverpool.ac.uk:3005780 2024-09-15T18:21:10+00:00 Observed Basin-Scale Response of the North Atlantic Meridional Overturning Circulation to Wind Stress Forcing Elipot, Shane Frajka-Williams, Eleanor Hughes, Chris W Olhede, Sofia Lankhorst, Matthias 2017 text https://livrepository.liverpool.ac.uk/3005780/ https://doi.org/10.1175/jcli-d-16-0664.1 https://livrepository.liverpool.ac.uk/3005780/1/Elipot_et_al_JClim_2017_accepted2016.pdf https://livrepository.liverpool.ac.uk/3005780/2/2017-Elipot_et_al_JClim_MOC_Basin_Scale_wind.pdf en eng American Meteorological Society https://livrepository.liverpool.ac.uk/3005780/1/Elipot_et_al_JClim_2017_accepted2016.pdf https://livrepository.liverpool.ac.uk/3005780/2/2017-Elipot_et_al_JClim_MOC_Basin_Scale_wind.pdf Elipot, Shane, Frajka-Williams, Eleanor, Hughes, Chris W, Olhede, Sofia and Lankhorst, Matthias (2017) Observed Basin-Scale Response of the North Atlantic Meridional Overturning Circulation to Wind Stress Forcing. JOURNAL OF CLIMATE, 30 (6). pp. 2029-2054. Article NonPeerReviewed 2017 ftunivliverpool https://doi.org/10.1175/jcli-d-16-0664.1 2024-07-08T14:17:39Z <jats:title>Abstract</jats:title> <jats:p>The response of the North Atlantic meridional overturning circulation (MOC) to wind stress forcing is investigated from an observational standpoint, using four time series of overturning transports below and relative to 1000 m, overlapping by 3.6 yr. These time series are derived from four mooring arrays located on the western boundary of the North Atlantic: the RAPID Western Atlantic Variability Experiment (WAVE) array (42.5°N), the Woods Hole Oceanographic Institution Line W array (39°N), RAPID–MOC/MOCHA (26.5°N), and the Meridional Overturning Variability Experiment (MOVE) array (16°N). Using modal decompositions of the analytic cross-correlation between transports and wind stress, the basin-scale wind stress is shown to significantly drive the MOC coherently at four latitudes, on the time scales available for this study. The dominant mode of covariance is interpreted as rapid barotropic oceanic adjustments to wind stress forcing, eventually forming two counterrotating Ekman overturning cells centered on the tropics and subtropical gyre. A second mode of covariance appears related to patterns of wind stress and wind stress curl associated with the North Atlantic Oscillation, spinning anomalous horizontal circulations that likely interact with topography to form overturning cells.</jats:p> Article in Journal/Newspaper North Atlantic North Atlantic oscillation The University of Liverpool Repository Journal of Climate 30 6 2029 2054
institution Open Polar
collection The University of Liverpool Repository
op_collection_id ftunivliverpool
language English
description <jats:title>Abstract</jats:title> <jats:p>The response of the North Atlantic meridional overturning circulation (MOC) to wind stress forcing is investigated from an observational standpoint, using four time series of overturning transports below and relative to 1000 m, overlapping by 3.6 yr. These time series are derived from four mooring arrays located on the western boundary of the North Atlantic: the RAPID Western Atlantic Variability Experiment (WAVE) array (42.5°N), the Woods Hole Oceanographic Institution Line W array (39°N), RAPID–MOC/MOCHA (26.5°N), and the Meridional Overturning Variability Experiment (MOVE) array (16°N). Using modal decompositions of the analytic cross-correlation between transports and wind stress, the basin-scale wind stress is shown to significantly drive the MOC coherently at four latitudes, on the time scales available for this study. The dominant mode of covariance is interpreted as rapid barotropic oceanic adjustments to wind stress forcing, eventually forming two counterrotating Ekman overturning cells centered on the tropics and subtropical gyre. A second mode of covariance appears related to patterns of wind stress and wind stress curl associated with the North Atlantic Oscillation, spinning anomalous horizontal circulations that likely interact with topography to form overturning cells.</jats:p>
format Article in Journal/Newspaper
author Elipot, Shane
Frajka-Williams, Eleanor
Hughes, Chris W
Olhede, Sofia
Lankhorst, Matthias
spellingShingle Elipot, Shane
Frajka-Williams, Eleanor
Hughes, Chris W
Olhede, Sofia
Lankhorst, Matthias
Observed Basin-Scale Response of the North Atlantic Meridional Overturning Circulation to Wind Stress Forcing
author_facet Elipot, Shane
Frajka-Williams, Eleanor
Hughes, Chris W
Olhede, Sofia
Lankhorst, Matthias
author_sort Elipot, Shane
title Observed Basin-Scale Response of the North Atlantic Meridional Overturning Circulation to Wind Stress Forcing
title_short Observed Basin-Scale Response of the North Atlantic Meridional Overturning Circulation to Wind Stress Forcing
title_full Observed Basin-Scale Response of the North Atlantic Meridional Overturning Circulation to Wind Stress Forcing
title_fullStr Observed Basin-Scale Response of the North Atlantic Meridional Overturning Circulation to Wind Stress Forcing
title_full_unstemmed Observed Basin-Scale Response of the North Atlantic Meridional Overturning Circulation to Wind Stress Forcing
title_sort observed basin-scale response of the north atlantic meridional overturning circulation to wind stress forcing
publisher American Meteorological Society
publishDate 2017
url https://livrepository.liverpool.ac.uk/3005780/
https://doi.org/10.1175/jcli-d-16-0664.1
https://livrepository.liverpool.ac.uk/3005780/1/Elipot_et_al_JClim_2017_accepted2016.pdf
https://livrepository.liverpool.ac.uk/3005780/2/2017-Elipot_et_al_JClim_MOC_Basin_Scale_wind.pdf
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation https://livrepository.liverpool.ac.uk/3005780/1/Elipot_et_al_JClim_2017_accepted2016.pdf
https://livrepository.liverpool.ac.uk/3005780/2/2017-Elipot_et_al_JClim_MOC_Basin_Scale_wind.pdf
Elipot, Shane, Frajka-Williams, Eleanor, Hughes, Chris W, Olhede, Sofia and Lankhorst, Matthias (2017) Observed Basin-Scale Response of the North Atlantic Meridional Overturning Circulation to Wind Stress Forcing. JOURNAL OF CLIMATE, 30 (6). pp. 2029-2054.
op_doi https://doi.org/10.1175/jcli-d-16-0664.1
container_title Journal of Climate
container_volume 30
container_issue 6
container_start_page 2029
op_container_end_page 2054
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