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Ocean Science An interactive open-access journal of the European Geosciences Union

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Ocean Sci., 13, 315-335, 2017
http://www.ocean-sci.net/13/315/2017/
doi:10.5194/os-13-315-2017
© Author(s) 2017. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
21 Apr 2017
Large-scale forcing of the European Slope Current and associated inflows to the North Sea
Robert Marsh et al.

Data sets

SSALTO/DUACS User Handbook: MSLA and (M)ADT Near-Real Time and Delayed Time Products, SALP-MU-P-EA-21065-CLS, CLS-DPS-NT-06-034 (5rev0, 20/08/2016)
AVISO+
http://www.aviso.altimetry.fr/fileadmin/documents/data/tools/hdbk_duacs.pdf
Kinematics of the Pacific Equatorial Undercurrent: a Eulerian and Lagrangian approach from GCM results
B. Blanke and S. Raynaud
http://stockage.univ-brest.fr/~grima/Ariane/doc.html
The ERA-Interim reanalysis: Configuration and performance of the data assimilation system (http://www.ecmwf.int/en/research/climate-reanalysis/era-interim)
D. P. Dee et al.
doi:10.1002/qj.828
Salinity Data
GODAS (NCEP Global Ocean Data Assimilation System)
https://www.esrl.noaa.gov/psd/data/gridded/data.godas.html
EN4: quality controlled ocean temperature and salinity profiles and monthly objective analyses with uncertainty estimates (http://www.metoffice.gov.uk/hadobs/en4/)
S. A. Good, M. J. Martin, and N. A. Rayner
doi:10.1002/2013JC009067
ICES Report on Ocean Climate 2015, ICES Cooperative Research Report No. 331
K. M. H. Larsen, C. Gonzalez-Pola, P. Fratantoni, A. Beszczynska-Möller, and S. L. Hughes (Eds.)
http://ocean.ices.dk/iroc/
Tide Gauge Data
PSMSL (Permanent Service for Mean Sea Level)
http://www.psmsl.org/data/obtaining/
Publications Copernicus
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Short summary
To the west of Britain and Ireland, a strong ocean current follows the steep slope that separates the deep Atlantic and the continental shelf. This “Slope Current” exerts an Atlantic influence on the North Sea and its ecosystems. Using a combination of computer modelling and archived data, we find that the Slope Current weakened over 1988–2007, reducing Atlantic influence on the North Sea, due to a combination of warming of the subpolar North Atlantic and weakening winds to the west of Scotland.
To the west of Britain and Ireland, a strong ocean current follows the steep slope that...
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