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• W2053131557 endingPage "106" @default.
• W2053131557 startingPage "81" @default.
• W2053131557 abstract "The role of deep-water formation and spreading as an indicator and regulator of global climatic change has recently been emphasized in a number of investigations (e.g. Watts & Hayder 1983, Boyle & Keigwin 1987, Labeyrie et al 1987, Anderson & Lundberg 1988). Within this context, processes in the Atlantic Ocean have attracted the greatest attention, since both the Norwegian and the Weddell Seas (which constitute the world’s two major areas where deep water is formed during wintertime convcction) are located on the margins of this ocean basin (Wrist 1936). The cold and dense water that fills the deeper parts of the Norwegian Sea escapes southward through two main passages: the Denmark Strait, and the Faroe Bank Channel. The deep-water outflow through the Denmark Strait (between Greenland and Iceland) over a comparatively shallow sill of depth ~ 600 m was known from the pioneering investigations at the turn of the century; it was, however, not studied in a systematic fashion until the 1960s (Mann 1969, Worthington 1969, Ross 1984). The existence of the Faroe Bank Channel, with a sill depth of 850 m, was unknown to Helland-Hansen & Nansen (1909), who stated that no bottom water with low temperatures can anywhere get out of the Norwegian" @default.
• W2053131557 created "2016-06-24" @default.
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• W2053131557 date "1991-01-01" @default.
• W2053131557 modified "2023-09-26" @default.
• W2053131557 title "Hydraulics of Rotating Strait and Sill Flow" @default.
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• W2053131557 doi "https://doi.org/10.1146/annurev.fl.23.010191.000501" @default.
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