2010
DOI: 10.1080/1755876x.2010.11020116
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The circulation pattern in the Mediterranean Sea: issues for modeller consideration

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Cited by 70 publications
(29 citation statements)
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“…Geographically, the Sicilian Channel splits the Mediterranean Sea into two different regions; the Western Basin and the Eastern Basin. The water circulation in the Mediterranean Sea is very complex due to i) several spatial and temporal processes that take place at all scales such as the excess of evaporation over precipitation, adjacent rivers runoff and intense topographic and coastal influences, and ii) the presence of three distinct water masses which flow independently throughout the whole Mediterranean Sea; the surface, the intermediate and the deep waters controlling the general circulation pattern (El-Geziry & Bryden, 2010 ;Waldman et al, 2018).…”
Section: Introductionmentioning
confidence: 99%
“…Geographically, the Sicilian Channel splits the Mediterranean Sea into two different regions; the Western Basin and the Eastern Basin. The water circulation in the Mediterranean Sea is very complex due to i) several spatial and temporal processes that take place at all scales such as the excess of evaporation over precipitation, adjacent rivers runoff and intense topographic and coastal influences, and ii) the presence of three distinct water masses which flow independently throughout the whole Mediterranean Sea; the surface, the intermediate and the deep waters controlling the general circulation pattern (El-Geziry & Bryden, 2010 ;Waldman et al, 2018).…”
Section: Introductionmentioning
confidence: 99%
“…Along the north coast of Algeria this current is of order 30–50 km wide and 200–400 m deep (near slope) with speeds of order 30–80 cm s −1 in the surface 100 m (Testor et al, ). As a result of barotropic and baroclinic instabilities meanders regularly form in this current (El‐Geziry & Bryden, ), which then typically spin off eddies of ~30 km diameter that circulate the Algerian Basin, following a cyclonic pathway (Cotroneo et al, ; Escudier et al, ; Testor et al, ). These contribute to an active mesoscale field in the central basin, which constitutes the second regime.…”
Section: Introductionmentioning
confidence: 99%
“… (a) Map and bathymetry of the western Pontine Islands (PO: Ponza, GA: Gavi, PA: Palmarola, ZA: Zannone). (b) Geographic location of the western Pontine Islands with the direction of the main marine currents in the Tyrrhenian Sea according to El-Geziry and Bryden 77 . (c) Statistical parsimony networks of the mtDNA ( cytb + nd4 ) and nuDNA ( mc1r and β -fibint7 ) fragments.…”
Section: Resultsmentioning
confidence: 99%