Multiple timescales of stochastically forced North Atlantic Ocean variability: A model study
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 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.
North Atlantic, NAO, Atlantic multidecadal variability, AMOC, Subpolar gyre, Stochastic, OGCM
1367-1381
Mecking, Jennifer V.
9b090069-5061-4340-b736-9690894ce203
Keenlyside, Noel S.
6e798056-cc0e-4c3c-a2e8-769a26922a2f
Greatbatch, Richard J.
1e4b74c6-29ec-4d21-877f-96350daadf60
September 2015
Mecking, Jennifer V.
9b090069-5061-4340-b736-9690894ce203
Keenlyside, Noel S.
6e798056-cc0e-4c3c-a2e8-769a26922a2f
Greatbatch, Richard J.
1e4b74c6-29ec-4d21-877f-96350daadf60
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), .
(doi:10.1007/s10236-015-0868-0).
Abstract
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.
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Published date: September 2015
Keywords:
North Atlantic, NAO, Atlantic multidecadal variability, AMOC, Subpolar gyre, Stochastic, OGCM
Organisations:
Physical Oceanography
Identifiers
Local EPrints ID: 383875
URI: http://eprints.soton.ac.uk/id/eprint/383875
ISSN: 1616-7341
PURE UUID: c331a8d6-b21e-4670-85c5-b1859a3b5eaf
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Date deposited: 10 Nov 2015 15:05
Last modified: 14 Mar 2024 21:49
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Contributors
Author:
Jennifer V. Mecking
Author:
Noel S. Keenlyside
Author:
Richard J. Greatbatch
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