2002
DOI: 10.1080/01431160110034681
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Observations of oceanic mesoscale features and variability in the Canary Islands area from ERS-1 altimeter data, satellite infrared imagery and hydrographic measurements

Abstract: The main purposes of this paper are to identify and evaluate the oceanic mesoscale features that appear in the Atlantic Ocean eastern boundary. 20-40° N, 19-9° W, using ERS-1 (1992-1993) satellite altimeter data. The sea surface height anomalies and the eddy kinetic energy fields are calculated. High energy values, between 0.03 and 0.05 m2 s-2, are observed with the altimeter data in the Canary region mainly in summer. These maximum values are associated with eddies located downstream of Gran Canaria and Tener… Show more

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Cited by 19 publications
(9 citation statements)
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“…They may appear rounded near islands or in the open ocean. In cool eddies, cold nutrient-rich water rises to the surface [25], while warm eddies (see Fig. 1) drag water with organic material to the ocean floor and keep in the warm surface.…”
Section: A Ocean Phenomenamentioning
confidence: 99%
See 1 more Smart Citation
“…They may appear rounded near islands or in the open ocean. In cool eddies, cold nutrient-rich water rises to the surface [25], while warm eddies (see Fig. 1) drag water with organic material to the ocean floor and keep in the warm surface.…”
Section: A Ocean Phenomenamentioning
confidence: 99%
“…In this area, there are many MOS throughout the year. Many works have described the MOS in this area [8], [22]- [25].…”
Section: A Ocean Phenomenamentioning
confidence: 99%
“…They may appear rounded near islands or in the open ocean. In cool eddies, cold nutrient-rich water rises to the surface [18], while warm eddies (see Fig. 1) drag water with organic material to the ocean floor and keep in the warm surface.…”
Section: Introductionmentioning
confidence: 99%
“…The zone selected for our study, the Northwest African area, presents conditions appropriate for the formation of MOS, such as upwellings, filaments, cold and warm eddies, and wakes, throughout the year (García-Weil et al (2000); Barton et al (1998); Arístegui et al (1994); Sangra et al (2005); Tejera et al (2002); Meunier et al (2012)) (see Figure 1).…”
Section: Introductionmentioning
confidence: 99%
“…In cool eddies, cold nutrient-rich water rises to the surface in counterclockwise swirls (Tejera et al (2002)). The opposite, warm eddies (see Figure 1), drag water with organic matter down to the ocean floor, leaving warm water on the surface, and are formed under stronger wind conditions.…”
Section: Introductionmentioning
confidence: 99%