The refraction, shoaling and structure of non-linear internal waves at a continental shelf margin
Observations of internal waves near the Continental shelf-edge are generally ascribed to generation by oscillating tidal flow over the local bathymetry, in the presence of a stratified water column, giving rise to the internal tide. In this thesis observations are presented which demonstrate that in...
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University of Southampton
2000
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.340340 |