Articles | Volume 12, issue 2
Ocean Sci., 12, 451–470, 2016
Ocean Sci., 12, 451–470, 2016

Research article 15 Mar 2016

Research article | 15 Mar 2016

Volume transport and mixing of the Faroe Bank Channel overflow from one year of moored measurements

Jenny E. Ullgren et al.

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Cited articles

Beaird, N. L., Fer, I., Rhines, P., and Eriksen, C.: Dissipation of turbulent kinetic energy inferred from Seagliders: an application to the Eastern Nordic Seas overflows, J. Phys. Oceanogr., 42, 2268–2282,, 2012.
Beaird, N. L., Rhines, P. B., and Eriksen, C. C.: Overflow waters at the Iceland-Faroe Ridge observed in multiyear Seaglider surveys, J. Phys. Oceanogr., 43, 2334–2351,, 2013.
Borenäs, K. and Lundberg, P.: The Faroe-Bank Channel deep-water overflow, Deep-Sea Res. Pt. II, 51, 335–350, 2004.
Borenäs, K. M. and Lundberg, P. A.: On the deep-water flow through the Faroe Bank Channel, J. Geophys. Res., 93, 1281–1292, 1988.
Borenäs, K. M., Lake, I. M., and Lundberg, P. A.: On the intermediate water masses of the Faroe-Bank Channel overflow, J. Phys. Oceanogr., 31, 1904–1914, 2001.
Short summary
One-year long moored measurements of currents and hydrographic properties in the overflow region of the Faroe Bank Channel have provided a more accurate observational-based estimate of the volume transport, entrainment, and eddy diffusivities associated with the overflow plume. The data set resolves the temporal variability and covers the entire lateral and vertical extent of the plume.