2020
DOI: 10.1016/j.pocean.2020.102271
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Islands as eddy transformation and generation hotspots: Cabo Verde case study

Abstract: The characterisation of incoming background and island-induced mesoscale eddies in the Cape Verde Archipelago is discussed herein. Special attention is given to the interaction of background eddies with the islands topography and orographic winds, along with the interaction and potential impacts on the generation of island-induced eddies. Some examples of the local biological response to background and island-induced eddies are given. This is achieved by combining remote-sensing satellite observations for wind… Show more

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Cited by 15 publications
(23 citation statements)
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“…Such dynamic variability at the Mauritania coast is expected to affect the Cabo Verde islands, located 450-600 km west. For example, filaments rich in Chlorophyll a have been observed to reach the archipelago during the upwelling season (Lathuilière et al, 2008;Ohde and Siegel, 2010), whereas eddies generated by the dynamic instabilities of the Mauritania Current (Lázaro et al, 2005) and by the interaction of coastal currents with topography (Schütte et al, 2016) are often blocked by the Cabo-Verdian islands as they propagate westward (Cardoso et al, 2020).…”
Section: Oceanographic Settingmentioning
confidence: 99%
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“…Such dynamic variability at the Mauritania coast is expected to affect the Cabo Verde islands, located 450-600 km west. For example, filaments rich in Chlorophyll a have been observed to reach the archipelago during the upwelling season (Lathuilière et al, 2008;Ohde and Siegel, 2010), whereas eddies generated by the dynamic instabilities of the Mauritania Current (Lázaro et al, 2005) and by the interaction of coastal currents with topography (Schütte et al, 2016) are often blocked by the Cabo-Verdian islands as they propagate westward (Cardoso et al, 2020).…”
Section: Oceanographic Settingmentioning
confidence: 99%
“…Three of the drifters leaving Canaries reach the Cabo Verde archipelago as they float in the easternmost branches of the Canary and North Equatorial Currents (Figures 3A, 1A), being the only common trajectories between Cabo Verde and the other archipelagos of the Macaronesia (Table 2). Although Cabo Verde lies at the southern limit of the North Atlantic Gyre, the archipelago is predominantly exposed to westward drifters released along the Northwestern African coast, most likely advected by the seasonal Mauritania Current (dashed arrow in Figure 1A; Lázaro et al, 2005), upwelling filaments (Lathuilière et al, 2008;Ohde and Siegel, 2010) or coastal-generated eddies (Schütte et al, 2016;Cardoso et al, 2020). Nevertheless, the eastward-flowing North Equatorial Counter Current can still be responsible for the advection of drifters released south of the archipelago.…”
Section: Drifter Trajectoriesmentioning
confidence: 99%
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