Multiple timescales of stochastically forced North Atlantic Ocean variability: A model study

The Atlantic meridional overturning circulation (AMOC) and the subpolar gyre (SPG) are important elements in mechanisms for multidecadal variability in models in the North Atlantic Ocean. In this study, a 2000-year long global ocean model integration forced with the atmospheric patterns associated w...

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Published in:Ocean Dynamics
Main Authors: Mecking, Jennifer V., Keenlyside, Noel S., Greatbatch, Richard J.
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
Online Access:https://eprints.soton.ac.uk/383875/
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spelling ftsouthampton:oai:eprints.soton.ac.uk:383875 2023-07-30T04:05:11+02:00 Multiple timescales of stochastically forced North Atlantic Ocean variability: A model study Mecking, Jennifer V. Keenlyside, Noel S. Greatbatch, Richard J. 2015-09 https://eprints.soton.ac.uk/383875/ English eng Mecking, Jennifer V., Keenlyside, Noel S. and Greatbatch, Richard J. (2015) Multiple timescales of stochastically forced North Atlantic Ocean variability: A model study. Ocean Dynamics, 65 (9-10), 1367-1381. (doi:10.1007/s10236-015-0868-0 <http://dx.doi.org/10.1007/s10236-015-0868-0>). Article PeerReviewed 2015 ftsouthampton https://doi.org/10.1007/s10236-015-0868-0 2023-07-09T22:02:48Z The Atlantic meridional overturning circulation (AMOC) and the subpolar gyre (SPG) are important elements in mechanisms for multidecadal variability in models in the North Atlantic Ocean. In this study, a 2000-year long global ocean model integration forced with the atmospheric patterns associated with a white noise North Atlantic Oscillation (NAO) index is shown to have three distinct timescales of North Atlantic Ocean variability. First, an interannual timescale with variability shorter than 15 years, that can be related to Ekman dynamics. Second, a multidecadal timescale, on the 15- to 65-year range, that is mainly concentrated in the SPG region and is controlled by constructive interference between density anomalies around the gyre and the changing NAO forcing. Finally, the centennial timescales, with variability longer than 65 years, that can be attributed to the ocean being in a series of quasi-equilibrium states. The relationship between the ocean’s response and the NAO index differs for each timescale; the 15-year and shorter timescales are directly related to the NAO of the same year, 15- to 65-year timescales are dependent on the NAO index in the last 25–30 years in a sinusoidal sense while the 65-year and longer timescales relate to a sum of the last 50–80 years of the NAO index. Article in Journal/Newspaper North Atlantic North Atlantic oscillation University of Southampton: e-Prints Soton Ocean Dynamics 65 9-10 1367 1381
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description The Atlantic meridional overturning circulation (AMOC) and the subpolar gyre (SPG) are important elements in mechanisms for multidecadal variability in models in the North Atlantic Ocean. In this study, a 2000-year long global ocean model integration forced with the atmospheric patterns associated with a white noise North Atlantic Oscillation (NAO) index is shown to have three distinct timescales of North Atlantic Ocean variability. First, an interannual timescale with variability shorter than 15 years, that can be related to Ekman dynamics. Second, a multidecadal timescale, on the 15- to 65-year range, that is mainly concentrated in the SPG region and is controlled by constructive interference between density anomalies around the gyre and the changing NAO forcing. Finally, the centennial timescales, with variability longer than 65 years, that can be attributed to the ocean being in a series of quasi-equilibrium states. The relationship between the ocean’s response and the NAO index differs for each timescale; the 15-year and shorter timescales are directly related to the NAO of the same year, 15- to 65-year timescales are dependent on the NAO index in the last 25–30 years in a sinusoidal sense while the 65-year and longer timescales relate to a sum of the last 50–80 years of the NAO index.
format Article in Journal/Newspaper
author Mecking, Jennifer V.
Keenlyside, Noel S.
Greatbatch, Richard J.
spellingShingle Mecking, Jennifer V.
Keenlyside, Noel S.
Greatbatch, Richard J.
Multiple timescales of stochastically forced North Atlantic Ocean variability: A model study
author_facet Mecking, Jennifer V.
Keenlyside, Noel S.
Greatbatch, Richard J.
author_sort Mecking, Jennifer V.
title Multiple timescales of stochastically forced North Atlantic Ocean variability: A model study
title_short Multiple timescales of stochastically forced North Atlantic Ocean variability: A model study
title_full Multiple timescales of stochastically forced North Atlantic Ocean variability: A model study
title_fullStr Multiple timescales of stochastically forced North Atlantic Ocean variability: A model study
title_full_unstemmed Multiple timescales of stochastically forced North Atlantic Ocean variability: A model study
title_sort multiple timescales of stochastically forced north atlantic ocean variability: a model study
publishDate 2015
url https://eprints.soton.ac.uk/383875/
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation Mecking, Jennifer V., Keenlyside, Noel S. and Greatbatch, Richard J. (2015) Multiple timescales of stochastically forced North Atlantic Ocean variability: A model study. Ocean Dynamics, 65 (9-10), 1367-1381. (doi:10.1007/s10236-015-0868-0 <http://dx.doi.org/10.1007/s10236-015-0868-0>).
op_doi https://doi.org/10.1007/s10236-015-0868-0
container_title Ocean Dynamics
container_volume 65
container_issue 9-10
container_start_page 1367
op_container_end_page 1381
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