Observations of small-scale secondary instabilities during the shoaling of internal bores on a deep-ocean slope
The Rockall Bank area, located in the north-east Atlantic Ocean, is a region dominated by topographically-trapped diurnal tides. These tides generate up-and down-slope displacements that can be locally described as swashing motions on the bank. Using high spatial and time resolution of moored temper...
| Published in: | Journal of Physical Oceanography |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
2016
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| Subjects: | |
| Online Access: | https://www.vliz.be/imisdocs/publications/35/299735.pdf |