The Barents Sea frontal zones and water masses variability (1980–2011)
The polar front separates the warm and saline Atlantic Water entering the southern Barents Sea from the cold and fresh Arctic Water located in the north. These water masses can mix together (mainly in the center of the Barents Sea), be cooled by the atmosphere and receive salt because of brine relea...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2016-01-01
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| Series: | Ocean Science |
| Online Access: | http://www.ocean-sci.net/12/169/2016/os-12-169-2016.pdf |
| _version_ | 1818148908890587136 |
|---|---|
| author | L. Oziel J. Sirven J.-C. Gascard |
| author_facet | L. Oziel J. Sirven J.-C. Gascard |
| author_sort | L. Oziel |
| collection | DOAJ |
| description | The polar front separates the warm and saline Atlantic Water entering the
southern Barents Sea from the cold and fresh Arctic Water located in the
north. These water masses can mix together (mainly in the center of the
Barents Sea), be cooled by the atmosphere and receive salt because of brine
release; these processes generate dense water in winter, which then cascades
into the Arctic Ocean to form the <i>Arctic Intermediate Water</i>. To
study the interannual variability and evolution of the frontal zones and the
corresponding variations of the water masses, we have merged data from the
International Council for the Exploration of the Sea and the Arctic and
Antarctic Research Institute and have built a new database, which covers the
1980–2011 period. The summer data were interpolated on a regular grid. A
<i>probability density function</i> is used to show that the polar front
splits into two branches east of 32° E where the topographic
constraint weakens. Two fronts can then be identified: the <i>Northern
Front</i> is associated with strong salinity gradients and the <i>Southern
Front</i> with temperature gradients. Both fronts enclose the denser Barents Sea
Water. The interannual variability of the water masses is apparent in the
observed data and is linked to that of the ice cover. The frontal zones
variability is found by using data from a general circulation model. The link
with the atmospheric variability, represented here by the Arctic Oscillation,
is not clear. However, model results suggest that such a link could be
validated if winter data were taken into account. A strong trend appears: the
Atlantic Water (Arctic Water) occupies a larger (smaller) volume of the
Barents Sea. This trend amplifies during the last decade and the model study
suggests that this could be accompanied by a northwards displacement of the
Southern Front in the eastern part of the Barents Sea. The results are less
clear for the Northern Front. The observations show that the volume of the
Barents Sea Water remains nearly unchanged, which suggests a northwards shift
of the Northern Front to compensate for the northward shift of the Southern
Front. Lastly, we noticed that the seasonal variability of the position of
the front is small. |
| first_indexed | 2024-12-11T12:58:37Z |
| format | Article |
| id | doaj.art-8357f9edd5ad47b68b47633b1ca4013f |
| institution | Directory Open Access Journal |
| issn | 1812-0784 1812-0792 |
| language | English |
| last_indexed | 2024-12-11T12:58:37Z |
| publishDate | 2016-01-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Ocean Science |
| spelling | doaj.art-8357f9edd5ad47b68b47633b1ca4013f2022-12-22T01:06:32ZengCopernicus PublicationsOcean Science1812-07841812-07922016-01-0112116918410.5194/os-12-169-2016The Barents Sea frontal zones and water masses variability (1980–2011)L. Oziel0J. Sirven1J.-C. Gascard2Sorbonne Universités (UPMC, Univ Paris 06)-CNRS-IRD-MNHN, LOCEAN Laboratory, IPSL, Université Pierre et Marie Curie, 75005, Paris, FranceSorbonne Universités (UPMC, Univ Paris 06)-CNRS-IRD-MNHN, LOCEAN Laboratory, IPSL, Université Pierre et Marie Curie, 75005, Paris, FranceSorbonne Universités (UPMC, Univ Paris 06)-CNRS-IRD-MNHN, LOCEAN Laboratory, IPSL, Université Pierre et Marie Curie, 75005, Paris, FranceThe polar front separates the warm and saline Atlantic Water entering the southern Barents Sea from the cold and fresh Arctic Water located in the north. These water masses can mix together (mainly in the center of the Barents Sea), be cooled by the atmosphere and receive salt because of brine release; these processes generate dense water in winter, which then cascades into the Arctic Ocean to form the <i>Arctic Intermediate Water</i>. To study the interannual variability and evolution of the frontal zones and the corresponding variations of the water masses, we have merged data from the International Council for the Exploration of the Sea and the Arctic and Antarctic Research Institute and have built a new database, which covers the 1980–2011 period. The summer data were interpolated on a regular grid. A <i>probability density function</i> is used to show that the polar front splits into two branches east of 32° E where the topographic constraint weakens. Two fronts can then be identified: the <i>Northern Front</i> is associated with strong salinity gradients and the <i>Southern Front</i> with temperature gradients. Both fronts enclose the denser Barents Sea Water. The interannual variability of the water masses is apparent in the observed data and is linked to that of the ice cover. The frontal zones variability is found by using data from a general circulation model. The link with the atmospheric variability, represented here by the Arctic Oscillation, is not clear. However, model results suggest that such a link could be validated if winter data were taken into account. A strong trend appears: the Atlantic Water (Arctic Water) occupies a larger (smaller) volume of the Barents Sea. This trend amplifies during the last decade and the model study suggests that this could be accompanied by a northwards displacement of the Southern Front in the eastern part of the Barents Sea. The results are less clear for the Northern Front. The observations show that the volume of the Barents Sea Water remains nearly unchanged, which suggests a northwards shift of the Northern Front to compensate for the northward shift of the Southern Front. Lastly, we noticed that the seasonal variability of the position of the front is small.http://www.ocean-sci.net/12/169/2016/os-12-169-2016.pdf |
| spellingShingle | L. Oziel J. Sirven J.-C. Gascard The Barents Sea frontal zones and water masses variability (1980–2011) Ocean Science |
| title | The Barents Sea frontal zones and water masses variability (1980–2011) |
| title_full | The Barents Sea frontal zones and water masses variability (1980–2011) |
| title_fullStr | The Barents Sea frontal zones and water masses variability (1980–2011) |
| title_full_unstemmed | The Barents Sea frontal zones and water masses variability (1980–2011) |
| title_short | The Barents Sea frontal zones and water masses variability (1980–2011) |
| title_sort | barents sea frontal zones and water masses variability 1980 2011 |
| url | http://www.ocean-sci.net/12/169/2016/os-12-169-2016.pdf |
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