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ICES ADVICE 2006 AVIS DU CIEM

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left panels). This ridge separates the Atlantic Ocean southwest of the ridge from the Norwegian Sea to the northeast. The sill of the ridge reaches different depths in different areas. Most of it is shallower than 500 m, but a small part is deeper with the Faroe Bank Channel being the deepest passage across the ridge. The upper layers of the waters surrounding the Faroes are dominated by ‘Modified North Atlantic Water’ which derives from the North Atlantic Current flowing towards the east and north-east (Hansen and Østerhus, 2000) (Figure 4.1.1.1, upper left panel). This water is typically around 8°C and salinities around 35.25. Deeper than...

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