Elsevier, Deep Sea Research Part I: Oceanographic Research Papers, (122), p. 48-59
DOI: 10.1016/j.dsr.2017.02.004
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Water mass analysis reveals a persistent core of deep overflow water within the Rockall Trough which hugs the northern and western boundaries of the basin. Mean speeds within this overflow are 10–15 cm s−1 giving a transport time from the Wyville Thomson Ridge to the central basin of