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- W2024806816 abstract "Two distinct classes of front coexist on the continental shelf west of Scotland in the vicinity of the island of Islay. The type I front forms the boundary of a low salinity coastal current in which the frontal interface extends continuously from the sea surface to the sea bed. The other (type II) front which develops in spring and summer marks the transition between mixed and thermally stratified water and is of the kind discussed by Simpson and Hunter (1974). The relative locations of the two frontal types changes with season. In winter, only the type I front is present. When thermal stratification commences in early spring a type II front forms to the west of the type I front. As thermal stratification develops farther, in late spring and summer, the type II front advances towards the type I system and eventually crosses it inducing a distortion of the type I interface and bringing about vertical haline stratification. In autumn it appears that the final breakdown of thermal stratification may be inhibited by the vertical salinity (density) gradient associated with the type I front." @default.
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- W2024806816 date "1989-05-01" @default.
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- W2024806816 title "On the interaction of thermal and haline fronts: The Islay front revisited" @default.
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- W2024806816 doi "https://doi.org/10.1016/0272-7714(89)90025-5" @default.
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