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Technical and physical challenges to achieve a regional simulation at multi-decadal scales: Applications to the Bay of Biscay. ArchiMer
Theetten, Sebastien; Vandermeirsch, Frederic; Assassi, Charefeddine; Charria, Guillaume.
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Ano: 2014 URL: http://archimer.ifremer.fr/doc/00195/30652/29120.pdf
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A first overview of the 53 year past hydrodynamical variability in the Bay of Biscay from a regional simulation ArchiMer
Charria, Guillaume; Vandermeirsch, Frederic; Theetten, Sebastien; Assassi, Charefeddine; Dussin, Raphael.
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Ano: 2014 URL: http://archimer.ifremer.fr/doc/00197/30786/29144.pdf
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Interannual variability of temperature over 50 years described by global simulation ArchiMer
Assassi, Charefeddine; Vandermeirsch, Frederic; Morel, Yves; Charria, Guillaume; Theetten, Sebastien; Dussin, Raphael; Molines, Jean-marc.
The aim of this study is to better understand the different overriding mechanisms that control the evolution of the temperature in the Bay of Biscay, through realistic simulations over a period of 50 years. Based on the work of Michel et al. (2009) on the variability of temperature in the Bay of Biscay (Fig1). We will extend the understanding of the interannual variability to the haline contents and the circulation at regional scale. Here we compare two global simulations, ORCA-G70 and ORCA-GRD100 (¼°resolution), that differs mainly in the vertical resolution and we show their variability.
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Ano: 2014 URL: http://archimer.ifremer.fr/doc/00197/30778/29137.pdf
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An index to distinguish surface and subsurface intensified vortices from surface observations ArchiMer
Assassi, Charefeddine; Morel, Y.; Vandermeirsch, Frederic; Chaigneau, A.; Pegliasco, C.; Morrow, R.; Colas, F.; Fleury, S.; Carton, Xavier; Klein, Patrice; Cambra, R..
In this study, we first show that it is difficult to reconstruct the vertical structure of vortices using only surface observations. In particular we show that the recent SQG and ISQG methods systematically lead to surface intensified vortices and those subsurface intensified vortices are thus not correctly modelled. We then investigate the possibility to distinguish between surface and subsurface intensified eddies from surface data only, using the sea surface height and the sea surface temperature available from satellite observations. A simple index, based on the ratio of the sea surface temperature anomaly and the sea level anomaly, is proposed. While the index is expected to give perfect results for isolated vortices, we show that in a complex...
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Ano: 2016 URL: https://archimer.ifremer.fr/doc/00343/45406/44921.pdf
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