Norwegian Sea overflow through the Faroe-Shetland gateway as documented by its bedforms
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 hierar...
Published in: | Marine Geology |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2002
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Subjects: | |
Online Access: | https://eprints.soton.ac.uk/43909/ |