Introduction and main ideas - RECYF Recherche et EXpérimentation sur les CYclogénèses et les Fronts

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Introduction and main ideas

Influence of Rossby wave-breaking on the North Atlantic Oscillation.

Jet streams in the upper troposphere usually reach their maximum on the western side of the oceanic basins where the land-sea thermal contrasts are the strongest. East of the same basins, synoptic eddies get larger amplitude and feedback onto the jet streams. This feedback (...)