Transports and pathways of overflow water in the Rockall Trough

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 <50 days. An...

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Bibliographic Details
Published in:Deep Sea Research Part I: Oceanographic Research Papers
Main Authors: Johnson, Clare, Sherwin, Toby, Cunningham, Stuart, Dumont, Estelle, Houpert, Loïc, Holliday, N. Penny
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:https://eprints.soton.ac.uk/406147/
https://eprints.soton.ac.uk/406147/1/1_s2.0_S0967063716302503_main.pdf