Volume exchange across the shelf edge : the role of the internal tide and other physical processes
The world ocean can broadly be split into two regimes, the shallow shelf seas up to a few hundred metres deep and the deep open ocean which is typically 4-5 km deep. These two regimes are separated by a narrow region of steep topography. This steep topography acts to limit the exchange to those proc...
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University of Liverpool
2017
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.722081 |