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A. Foussard, G. Lapeyre, and R. Plougonven

( Chelton et al. 2001 , 2004 ; O’Neill et al. 2003 ). It was also revealed through the signature of ocean eddies in turbulent air–sea fluxes of sensible and latent heat ( Bourras et al. 2004 ), or in cloud cover and rain rates ( Frenger et al. 2013 ). The coupling between the atmosphere and narrow oceanic structures has been explored through various analyses of the horizontal momentum budget in the boundary layer based on theoretical models ( Samelson et al. 2006 ; Schneider and Qiu 2015 ) or

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