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We have used seabed information from three deep-tow side-scan sonar surveys in order to trace the high-energy current core of Norwegian Sea Overflow Water (NSOW) from the Faroe-Shetland Channel (FSC) through the Faroe Bank Channel (FBC) towards the southern flank of the Iceland-Faroe Ridge. A hierarchy of bedform types was used for estimating maximum mean near-bottom current speed, which has been...
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