Intrinsic variability of the Atlantic Meridional Overturning Circulation at interannual-to-multidecadal time scales
The low-frequency variability of the Atlantic meridional overturning circulation (AMOC) is investigated from 2, ¼°, and ° global ocean–sea ice simulations, with a specific focus on its internally generated (i.e., “intrinsic”) component. A 327-yr climatological ¼° simulation, driven by a repeated sea...
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ftsouthampton:oai:eprints.soton.ac.uk:380277 2023-07-30T04:05:33+02:00 Intrinsic variability of the Atlantic Meridional Overturning Circulation at interannual-to-multidecadal time scales Grégorio, Sandy Penduff, Thierry Sérazin, Guillaume Molines, Jean-Marc Barnier, Bernard Hirschi, Joël 2015-07 text https://eprints.soton.ac.uk/380277/ https://eprints.soton.ac.uk/380277/1/jpo-d-14-0163%25252E1.pdf en English eng https://eprints.soton.ac.uk/380277/1/jpo-d-14-0163%25252E1.pdf Grégorio, Sandy, Penduff, Thierry, Sérazin, Guillaume, Molines, Jean-Marc, Barnier, Bernard and Hirschi, Joël (2015) Intrinsic variability of the Atlantic Meridional Overturning Circulation at interannual-to-multidecadal time scales. Journal of Physical Oceanography, 45 (7), 1929-1946. (doi:10.1175/JPO-D-14-0163.1 <http://dx.doi.org/10.1175/JPO-D-14-0163.1>). Article PeerReviewed 2015 ftsouthampton https://doi.org/10.1175/JPO-D-14-0163.1 2023-07-09T22:00:50Z The low-frequency variability of the Atlantic meridional overturning circulation (AMOC) is investigated from 2, ¼°, and ° global ocean–sea ice simulations, with a specific focus on its internally generated (i.e., “intrinsic”) component. A 327-yr climatological ¼° simulation, driven by a repeated seasonal cycle (i.e., a forcing devoid of interannual time scales), is shown to spontaneously generate a significant fraction R of the interannual-to-decadal AMOC variance obtained in a 50-yr “fully forced” hindcast (with reanalyzed atmospheric forcing including interannual time scales). This intrinsic variance fraction R slightly depends on whether AMOCs are computed in geopotential or density coordinates, and on the period considered in the climatological simulation, but the following features are quite robust when mesoscale eddies are simulated (at both ¼° and ° resolutions); R barely exceeds 5%–10% in the subpolar gyre but reaches 30%–50% at 34°S, up to 20%–40% near 25°N, and 40%–60% near the Gulf Stream. About 25% of the meridional heat transport interannual variability is attributed to intrinsic processes at 34°S and near the Gulf Stream. Fourier and wavelet spectra, built from the 327-yr ¼° climatological simulation, further indicate that spectral peaks of intrinsic AMOC variability (i) are found at specific frequencies ranging from interannual to multidecadal, (ii) often extend over the whole meridional scale of gyres, (iii) stochastically change throughout these 327 yr, and (iv) sometimes match the spectral peaks found in the fully forced hindcast in the North Atlantic. Intrinsic AMOC variability is also detected at multidecadal time scales, with a marked meridional coherence between 35°S and 25°N (15–30 yr periods) and throughout the whole basin (50–90-yr periods). Article in Journal/Newspaper North Atlantic Sea ice University of Southampton: e-Prints Soton Journal of Physical Oceanography 45 7 1929 1946 |
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Open Polar |
collection |
University of Southampton: e-Prints Soton |
op_collection_id |
ftsouthampton |
language |
English |
description |
The low-frequency variability of the Atlantic meridional overturning circulation (AMOC) is investigated from 2, ¼°, and ° global ocean–sea ice simulations, with a specific focus on its internally generated (i.e., “intrinsic”) component. A 327-yr climatological ¼° simulation, driven by a repeated seasonal cycle (i.e., a forcing devoid of interannual time scales), is shown to spontaneously generate a significant fraction R of the interannual-to-decadal AMOC variance obtained in a 50-yr “fully forced” hindcast (with reanalyzed atmospheric forcing including interannual time scales). This intrinsic variance fraction R slightly depends on whether AMOCs are computed in geopotential or density coordinates, and on the period considered in the climatological simulation, but the following features are quite robust when mesoscale eddies are simulated (at both ¼° and ° resolutions); R barely exceeds 5%–10% in the subpolar gyre but reaches 30%–50% at 34°S, up to 20%–40% near 25°N, and 40%–60% near the Gulf Stream. About 25% of the meridional heat transport interannual variability is attributed to intrinsic processes at 34°S and near the Gulf Stream. Fourier and wavelet spectra, built from the 327-yr ¼° climatological simulation, further indicate that spectral peaks of intrinsic AMOC variability (i) are found at specific frequencies ranging from interannual to multidecadal, (ii) often extend over the whole meridional scale of gyres, (iii) stochastically change throughout these 327 yr, and (iv) sometimes match the spectral peaks found in the fully forced hindcast in the North Atlantic. Intrinsic AMOC variability is also detected at multidecadal time scales, with a marked meridional coherence between 35°S and 25°N (15–30 yr periods) and throughout the whole basin (50–90-yr periods). |
format |
Article in Journal/Newspaper |
author |
Grégorio, Sandy Penduff, Thierry Sérazin, Guillaume Molines, Jean-Marc Barnier, Bernard Hirschi, Joël |
spellingShingle |
Grégorio, Sandy Penduff, Thierry Sérazin, Guillaume Molines, Jean-Marc Barnier, Bernard Hirschi, Joël Intrinsic variability of the Atlantic Meridional Overturning Circulation at interannual-to-multidecadal time scales |
author_facet |
Grégorio, Sandy Penduff, Thierry Sérazin, Guillaume Molines, Jean-Marc Barnier, Bernard Hirschi, Joël |
author_sort |
Grégorio, Sandy |
title |
Intrinsic variability of the Atlantic Meridional Overturning Circulation at interannual-to-multidecadal time scales |
title_short |
Intrinsic variability of the Atlantic Meridional Overturning Circulation at interannual-to-multidecadal time scales |
title_full |
Intrinsic variability of the Atlantic Meridional Overturning Circulation at interannual-to-multidecadal time scales |
title_fullStr |
Intrinsic variability of the Atlantic Meridional Overturning Circulation at interannual-to-multidecadal time scales |
title_full_unstemmed |
Intrinsic variability of the Atlantic Meridional Overturning Circulation at interannual-to-multidecadal time scales |
title_sort |
intrinsic variability of the atlantic meridional overturning circulation at interannual-to-multidecadal time scales |
publishDate |
2015 |
url |
https://eprints.soton.ac.uk/380277/ https://eprints.soton.ac.uk/380277/1/jpo-d-14-0163%25252E1.pdf |
genre |
North Atlantic Sea ice |
genre_facet |
North Atlantic Sea ice |
op_relation |
https://eprints.soton.ac.uk/380277/1/jpo-d-14-0163%25252E1.pdf Grégorio, Sandy, Penduff, Thierry, Sérazin, Guillaume, Molines, Jean-Marc, Barnier, Bernard and Hirschi, Joël (2015) Intrinsic variability of the Atlantic Meridional Overturning Circulation at interannual-to-multidecadal time scales. Journal of Physical Oceanography, 45 (7), 1929-1946. (doi:10.1175/JPO-D-14-0163.1 <http://dx.doi.org/10.1175/JPO-D-14-0163.1>). |
op_doi |
https://doi.org/10.1175/JPO-D-14-0163.1 |
container_title |
Journal of Physical Oceanography |
container_volume |
45 |
container_issue |
7 |
container_start_page |
1929 |
op_container_end_page |
1946 |
_version_ |
1772817529558794240 |