摘要: Based on a reanalysis of the data from Gulf Stream ’60 survey I propose that Slope Water is comprised two distinct zones. The first, warm Water, well-mixed zone found between 0 and 400 m depth close to Stream; flow primarily eastward. second zone, Labrador deeper, clings continental slope below 100 m broadest near σt = 27.5; it poorly mixed flows west. boundary zones varies in shape intensity response changes Current. Observations made region south Halifax November 1973 are discussed terms In particular, movements examined.
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