Articles | Volume 12, issue 1
https://doi.org/10.5194/os-12-169-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/os-12-169-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The Barents Sea frontal zones and water masses variability (1980–2011)
L. Oziel
CORRESPONDING AUTHOR
Sorbonne Universités (UPMC, Univ Paris
06)-CNRS-IRD-MNHN, LOCEAN Laboratory, IPSL, Université Pierre et Marie
Curie, 75005, Paris, France
J. Sirven
Sorbonne Universités (UPMC, Univ Paris
06)-CNRS-IRD-MNHN, LOCEAN Laboratory, IPSL, Université Pierre et Marie
Curie, 75005, Paris, France
J.-C. Gascard
Sorbonne Universités (UPMC, Univ Paris
06)-CNRS-IRD-MNHN, LOCEAN Laboratory, IPSL, Université Pierre et Marie
Curie, 75005, Paris, France
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- Boreal marine fauna from the Barents Sea disperse to Arctic Northeast Greenland A. Andrews et al. 10.1038/s41598-019-42097-x
- Arctic Climate Change, Economy and Society (ACCESS): Integrated perspectives A. Crépin et al. 10.1007/s13280-017-0953-3
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Short summary
The Barents Sea (BS) is a subpolar region and a zone transition where the Atlantic and the Arctic water masses meets and creates the "Polar Front". This study, based on one of the largest hydrological data set, showed for the first time that the "Polar Front" splits into two branches in the eastern part of the BS. This study also showed that, in a context of climate change, the BS experiences an "Atlantification", which goes along with a north-eastward shift of the frontal structure.
The Barents Sea (BS) is a subpolar region and a zone transition where the Atlantic and the...