Editorial Type:
Article
Article Type:
Research Article

Intrinsic Variability of Sea Level from Global Ocean Simulations: Spatiotemporal Scales

Guillaume Sérazin CNRS, LGGE (UMR5183), Grenoble, and, Sciences de l’Univers au CERFACS, CERFACS/CNRS, URA1857, Université Paul Sabatier, Toulouse, France

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Thierry Penduff CNRS, Université Grenoble Alpes, LGGE (UMR5183), Grenoble, France

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Sandy Grégorio CNRS, Université Grenoble Alpes, LGGE (UMR5183), Grenoble, France

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Bernard Barnier CNRS, Université Grenoble Alpes, LGGE (UMR5183), Grenoble, France

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Jean-Marc Molines CNRS, Université Grenoble Alpes, LGGE (UMR5183), Grenoble, France

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Laurent Terray Sciences de l’Univers au CERFACS, CERFACS/CNRS, URA1857, Toulouse, France

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Print Publication:
15 May 2015
DOI:
https://doi.org/10.1175/JCLI-D-14-00554.1
Page(s):
4279–4292
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Abstract

In high-resolution ocean general circulation models (OGCMs), as in process-oriented models, a substantial amount of interannual to decadal variability is generated spontaneously by oceanic nonlinearities: that is, without any variability in the atmospheric forcing at these time scales. The authors investigate the temporal and spatial scales at which this intrinsic oceanic variability has the strongest imprints on sea level anomalies (SLAs) using a ° global OGCM, by comparing a “hindcast” driven by the full range of atmospheric time scales with its counterpart forced by a repeated climatological atmospheric seasonal cycle. Outputs from both simulations are compared within distinct frequency–wavenumber bins. The fully forced hindcast is shown to reproduce the observed distribution and magnitude of low-frequency SLA variability very accurately. The small-scale (L < 6°) SLA variance is, at all time scales, barely sensitive to atmospheric variability and is almost entirely of intrinsic origin. The high-frequency (mesoscale) part and the low-frequency part of this small-scale variability have almost identical geographical distributions, supporting the hypothesis of a nonlinear temporal inverse cascade spontaneously transferring kinetic energy from high to low frequencies. The large-scale (L > 12°) low-frequency variability is mostly related to the atmospheric variability over most of the global ocean, but it is shown to remain largely intrinsic in three eddy-active regions: the Gulf Stream, Kuroshio, and Antarctic Circumpolar Current (ACC). Compared to its ¼° predecessor, the authors’ ° OGCM is shown to yield a stronger intrinsic SLA variability, at both mesoscale and low frequencies.

Denotes Open Access content.

Publisher’s Note: This article was revised on 10 June 2015 to correct a typographical error in the abstract where the wrong inequality was used, and to update the Grégorio et al. (2014) reference throughout the article to Grégorio et al. (2015).

Corresponding author address: Guillaume Sérazin, Laboratoire de Glaciologie et Géophysique de l’Environnement LGGE/CNRS, BP 96, 38402 Saint-Martin d’Heres, Grenoble, France. E-mail: guillaume.serazin@legi.grenoble-inp.fr

Abstract

In high-resolution ocean general circulation models (OGCMs), as in process-oriented models, a substantial amount of interannual to decadal variability is generated spontaneously by oceanic nonlinearities: that is, without any variability in the atmospheric forcing at these time scales. The authors investigate the temporal and spatial scales at which this intrinsic oceanic variability has the strongest imprints on sea level anomalies (SLAs) using a ° global OGCM, by comparing a “hindcast” driven by the full range of atmospheric time scales with its counterpart forced by a repeated climatological atmospheric seasonal cycle. Outputs from both simulations are compared within distinct frequency–wavenumber bins. The fully forced hindcast is shown to reproduce the observed distribution and magnitude of low-frequency SLA variability very accurately. The small-scale (L < 6°) SLA variance is, at all time scales, barely sensitive to atmospheric variability and is almost entirely of intrinsic origin. The high-frequency (mesoscale) part and the low-frequency part of this small-scale variability have almost identical geographical distributions, supporting the hypothesis of a nonlinear temporal inverse cascade spontaneously transferring kinetic energy from high to low frequencies. The large-scale (L > 12°) low-frequency variability is mostly related to the atmospheric variability over most of the global ocean, but it is shown to remain largely intrinsic in three eddy-active regions: the Gulf Stream, Kuroshio, and Antarctic Circumpolar Current (ACC). Compared to its ¼° predecessor, the authors’ ° OGCM is shown to yield a stronger intrinsic SLA variability, at both mesoscale and low frequencies.

Denotes Open Access content.

Publisher’s Note: This article was revised on 10 June 2015 to correct a typographical error in the abstract where the wrong inequality was used, and to update the Grégorio et al. (2014) reference throughout the article to Grégorio et al. (2015).

Corresponding author address: Guillaume Sérazin, Laboratoire de Glaciologie et Géophysique de l’Environnement LGGE/CNRS, BP 96, 38402 Saint-Martin d’Heres, Grenoble, France. E-mail: guillaume.serazin@legi.grenoble-inp.fr
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