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Oceanic control of multidecadal variability in an idealized coupled GCM ArchiMer
Jamet, Quentin; Huck, Thierry; Arzel, Olivier; Campin, Jean-michel; De Verdiere, Alain Colin.
Idealized ocean models are known to develop intrinsic multidecadal oscillations of the meridional overturning circulation (MOC). Here we explore the role of ocean–atmosphere interactions on this low-frequency variability. We use a coupled ocean–atmosphere model set up in a flat-bottom aquaplanet geometry with two meridional boundaries. The model is run at three different horizontal resolutions (4°, 2° and 1°) in both the ocean and atmosphere. At all resolutions, the MOC exhibits spontaneous variability on multidecadal timescales in the range 30–40 years, associated with the propagation of large-scale baroclinic Rossby waves across the Atlantic-like basin. The unstable region of growth of these waves through the long wave limit of baroclinic instability...
Tipo: Text Palavras-chave: Atlantic multidecadal oscillation; Air-sea interactions; NAO; Rossby waves; Idealized configuration.
Ano: 2016 URL: http://archimer.ifremer.fr/doc/00334/44483/44197.pdf
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Open ocean regimes of relative dispersion ArchiMer
Ollitrault, Michel; Gabillet, Céline; De Verdiere, Alain Colin.
As two fluid particles separate in time, the entire spectrum of eddy motions is being sampled from the smallest to the largest scales. In large-scale geophysical systems for which the Earth rotation is important, it has been conjectured that the relative diffusivity should vary respectively as D-2 and D-4/3 for distances respectively smaller and larger than a well-defined forcing scale of the order of the internal Rossby radius (with D the r.m.s. separation distance). Particle paths data from a mid-latitude float experiment in the central part of the North Atlantic appear to support these statements partly: two particles initially separated by a few km within two distinct clusters west and east of the mid-Atlantic ridge, statistically dispersed following a...
Tipo: Text Palavras-chave: Taylor dispersion; Dispersion; Atlantic circulation; Particule pairs.
Ano: 2005 URL: http://archimer.ifremer.fr/doc/2005/publication-456.pdf
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A direct determination of the World Ocean barotropic circulation ArchiMer
De Verdiere, Alain Colin; Ollitrault, Michel.
The time-mean Argo float displacements and the World Ocean Atlas 2009 temperature–salinity climatology are used to obtain the total, top to bottom, mass transports. Outside of an equatorial band, the total transports are the sum of the vertical integrals of geostrophic- and wind-driven Ekman currents. However, these transports are generally divergent, and to obtain a mass conserving circulation, a Poisson equation is solved for the streamfunction with Dirichlet boundary conditions at solid boundaries. The value of the streamfunction on islands is also part of the unknowns. This study presents and discusses an energetic circulation in three basins: the North Atlantic, the North Pacific, and the Southern Ocean. This global method leads to new estimations of...
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Ano: 2016 URL: http://archimer.ifremer.fr/doc/00309/42033/41332.pdf
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