Now showing items 1-3 of 3
Passive tracers and active dynamics - a model study of hydrography and circulation in the northern North Atlantic
(American Geophysical Union, 2006-08)
A long-standing problem in oceanography has been to understand the relationship between what can be measured in the ocean, such as hydrography, and what cannot, such as the strength and structure of the complete ...
Observations of highly regular oscillations in the overflow plume downstream of the Faroe Bank Channel
The Faroe Bank Channel (FBC) is the deepest connection between the Atlantic Ocean and the Nordic Seas. This work describes the dynamic properties of the plume of dense overflow water descending from the Faroe Bank ...
North Sea circulation: Atlantic inflow and its destination
(American Geophysical Union, 2006-12-22)
This study investigates the Atlantic inflow to the North Sea; its variabil- ity, pathways and destination. Results from a numerical model show that the variability of Atlantic inflow is dependent on the inflow location. ...