Impact of Ekman Pumping on the Meridional Coherence of the AMOC

Abstract The effect of wind‐induced vertical velocity on the meridional coherence of Atlantic meridional overtuning circulation (AMOC) is examined using theory, observations, and a numerical model. Two cases are considered: (a) the AMOC computed in depth coordinates and (b) the AMOC computed in isop...

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Main Authors: Neil J. Fraser, Alan D. Fox, Stuart A. Cunningham
Format: Article
Language:English
Published: Wiley 2025-01-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2024GL108846
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author Neil J. Fraser
Alan D. Fox
Stuart A. Cunningham
author_facet Neil J. Fraser
Alan D. Fox
Stuart A. Cunningham
author_sort Neil J. Fraser
collection DOAJ
description Abstract The effect of wind‐induced vertical velocity on the meridional coherence of Atlantic meridional overtuning circulation (AMOC) is examined using theory, observations, and a numerical model. Two cases are considered: (a) the AMOC computed in depth coordinates and (b) the AMOC computed in isopycnal coordinates. In depth space, the difference between the AMOC at different latitudes is largely explained by vertical transport across the 1000m depth surface induced by Ekman pumping. In density space, this difference is explained by Ekman‐driven heave of the neutral surface separating the upper and lower limbs. This adiabatic “sloshing” changes the relative volumes of the upper and lower AMOC limbs, obscuring the distribution and advection of the diapycnal transports which characterize the AMOC.
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series Geophysical Research Letters
spelling doaj-art-a78ad87fd91a4f7e97968eb867dff54b2025-01-20T13:05:57ZengWileyGeophysical Research Letters0094-82761944-80072025-01-01521n/an/a10.1029/2024GL108846Impact of Ekman Pumping on the Meridional Coherence of the AMOCNeil J. Fraser0Alan D. Fox1Stuart A. Cunningham2The Scottish Association for Marine Science Oban UKThe Scottish Association for Marine Science Oban UKThe Scottish Association for Marine Science Oban UKAbstract The effect of wind‐induced vertical velocity on the meridional coherence of Atlantic meridional overtuning circulation (AMOC) is examined using theory, observations, and a numerical model. Two cases are considered: (a) the AMOC computed in depth coordinates and (b) the AMOC computed in isopycnal coordinates. In depth space, the difference between the AMOC at different latitudes is largely explained by vertical transport across the 1000m depth surface induced by Ekman pumping. In density space, this difference is explained by Ekman‐driven heave of the neutral surface separating the upper and lower limbs. This adiabatic “sloshing” changes the relative volumes of the upper and lower AMOC limbs, obscuring the distribution and advection of the diapycnal transports which characterize the AMOC.https://doi.org/10.1029/2024GL108846AMOCclimateAtlanticOSNAPRAPIDcontinuity
spellingShingle Neil J. Fraser
Alan D. Fox
Stuart A. Cunningham
Impact of Ekman Pumping on the Meridional Coherence of the AMOC
Geophysical Research Letters
AMOC
climate
Atlantic
OSNAP
RAPID
continuity
title Impact of Ekman Pumping on the Meridional Coherence of the AMOC
title_full Impact of Ekman Pumping on the Meridional Coherence of the AMOC
title_fullStr Impact of Ekman Pumping on the Meridional Coherence of the AMOC
title_full_unstemmed Impact of Ekman Pumping on the Meridional Coherence of the AMOC
title_short Impact of Ekman Pumping on the Meridional Coherence of the AMOC
title_sort impact of ekman pumping on the meridional coherence of the amoc
topic AMOC
climate
Atlantic
OSNAP
RAPID
continuity
url https://doi.org/10.1029/2024GL108846
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