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- W2019921127 abstract "Accumulating evidence has pointed to a source of Northeast Atlantic Deep Water in the northern Rockall Trough and prompted a re-examination of geological and hydrographic data. The first showed that the sedimentary Feni Ridge could be traced along the length of the westernRockall Through to the foot of the Wyville-Thomson Ridge, and the second that dense water frequently existed at the lowest point of the ridge crest. Collected soundings and new data suggested a path by which this might enter the Rockall Trough, and overflow of Norweigian Sea Deep Water was observed taking place from the ridge crest in a narrow layer in July 1972. The flow is probably intermittent and appears to entrain Atlantic Water from intermediate depths." @default.
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- W2019921127 date "1973-09-01" @default.
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- W2019921127 title "The overflow of Norwegian sea deep water across the wyville-thomson Ridge" @default.
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- W2019921127 doi "https://doi.org/10.1016/0011-7471(73)90004-1" @default.
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