Articles | Volume 6, issue 4
https://doi.org/10.5194/os-6-901-2010
© Author(s) 2010. This work is distributed under the Creative Commons Attribution 3.0 License.
22 Oct 2010
A quantitative description of the Norwegian Atlantic Current by combining altimetry and hydrography
Related subject area
Depth range: All Depths | Approach: In situ Observations | Geographical range: Nordic Seas | Phenomena: Current Field
Overflow of cold water across the Iceland–Faroe Ridge through the Western Valley
Volume transport and mixing of the Faroe Bank Channel overflow from one year of moored measurements
On the modulation of the periodicity of the Faroe Bank Channel overflow instabilities
Ocean Sci., 14, 871–885, 2018
Ocean Sci., 12, 451–470, 2016
Ocean Sci., 11, 855–871, 2015
Cited articles
Bevington, P. R.: Data Reduction and Error Analysis for the Physical Science, McGraw-Hill Book Company, New York, USA, 1969.
Bochkov, Y. A.: Water temperature in the 0–200 m layer in the Kola-Meridian section in the Barents Sea, 1900–1981, Sb. Nauchn. Trud. PINRO, 46, 113–122, 1982.
Ducet, N., LeTraon, P. Y., and Reverdin, G.: Global high-resolution mapping of ocean circulation from TOPEX/Poseidon and ERS-1 and 2, J. Geophys. Res., 105, 19477–19498, 2000.
Gordon, R. L. and Huthnance, J.: Storm-driven continental shelf waves over the Scottish continental shelf, Cont. Shelf Res., 7, 1015–1048, 1987.
Häkkinen, S. and Rhines, P. B.: Decline of Subpolar North Atlantic Circulation During the 1990s, Science, 304, 555–559, 2004.
