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| Titel |
The circulation of Icelandic waters – a modelling study |
| VerfasserIn |
K. Logemann, J. Olafsson, Á. Snorrason, H. Valdimarsson, G. Marteinsdóttir |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1812-0784
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| Digitales Dokument |
URL |
| Erschienen |
In: Ocean Science ; 9, no. 5 ; Nr. 9, no. 5 (2013-10-30), S.931-955 |
| Datensatznummer |
250085250
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| Publikation (Nr.) |
 copernicus.org/os-9-931-2013.pdf |
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| Zusammenfassung |
| The three-dimensional flow, temperature and salinity fields of the North
Atlantic, including the Arctic Ocean, covering the time period 1992 to 2006 are
simulated with the numerical ocean model CODE. The simulation reveals several
new insights and previously unknown structures which help us to clarify open
questions on the regional oceanography of Icelandic waters. These relate to
the structure and geographical distribution of the coastal current, the
primary forcing of the North Icelandic Irminger Current (NIIC) and the path
of the Atlantic Water south-east of Iceland. The model's adaptively refined
computational mesh has a maximum resolution of 1 km horizontal and 2.5 m
vertical in Icelandic waters. CTD profiles from this region and the river
discharge of 46 Icelandic watersheds, computed by the hydrological model
WaSiM, are assimilated into the simulation. The model realistically
reproduces the established elements of the circulation around Iceland.
However, analysis of the simulated mean flow field also provides further
insights. It suggests a distinct freshwater-induced coastal current that only
exists along the south-west and west coasts, which is accompanied by a
counter-directed undercurrent. The simulated transport of Atlantic Water over
the Icelandic shelf takes place in a symmetrical system of two currents, with
the established NIIC over the north-western and northern shelf, and a
hitherto unnamed current over the southern and south-eastern shelf, which is
simulated to be an upstream precursor of the Faroe Current (FC). Both
currents are driven by barotropic pressure gradients induced by a sea level
slope across the Greenland–Scotland Ridge. The recently discovered North
Icelandic Jet (NIJ) also features in the model predictions and is found to be
forced by the baroclinic pressure field of the Arctic Front, to originate
east of the Kolbeinsey Ridge and to have a volume transport of around 1.5 Sv
within northern Denmark Strait. The simulated multi-annual mean Atlantic
Water transport of the NIIC increased by 85% during 1992 to 2006,
whereas the corresponding NIJ transport decreased by 27%. Based on our
model results we propose a new and further differentiated circulation scheme
of Icelandic waters whose details may inspire future observational
oceanography studies. |
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