Arctic layer salinity controls heat loss from deep Atlantic layer in seasonally ice‐covered areas of the Barents Sea
Abstract In the seasonally ice‐covered northern Barents Sea an intermediate layer of cold and relatively fresh Arctic Water at ~25–110 m depth isolates the sea surface and ice cover from a layer of warm and saline Atlantic Water below, a situation that resembles the cold halocline layer in the Euras...
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| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Wiley
2016-05-01
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| Series: | Geophysical Research Letters |
| Subjects: | |
| Online Access: | https://doi.org/10.1002/2016GL068421 |
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