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Eddy Topography Interactions on Eastern boundaries. Arnaud Le Boyer – Guillaume Roullet LPO, Brest. Dataset : « Bord Est » experiment 7 moorings / several depths Iberian margin 1 yr long 1989-1990. u. v. Typical KE spectrum. Tidal peaks. High-frequency : gravity waves. Mean flow.
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Eddy Topography Interactionson Eastern boundaries Arnaud Le Boyer – Guillaume Roullet LPO, Brest
Dataset : « Bord Est » experiment • 7 moorings / several depths • Iberian margin • 1 yr long 1989-1990 u v
Typical KE spectrum Tidal peaks High-frequency : gravity waves Mean flow Sub inertial range : T >> 1/f Coastal trapped waves (CTW)
Questions: • What is the forcing mechanism for this subinertial range [2days - 80days] ? • Wind • Eddy induced ? • How is this turbulence over the slope related to the mesoscale turbulence ?
Eddy-topography interaction • Mean current = Neptune effect • Transients ? Sketch of the coupling mechanism between eddies and CTW topography tends to force circulation along iso-f/H, associated transients = CTW
Collaboration with DRAKKAR • Investigate this issue within realistic, high resolution (1/12) simulations • Compare spectra on slope to spectra offshore • Relative contributions wind vs. Eddies on transients currents • Need for Eulerian time series along continental margins