Abstract
The winter of 2012 experienced peculiar atmospheric conditions that triggered a massive formation of dense water on the continental shelf and in the deep basin of the Gulf of Lions. Multiplatforms observations enabled a synoptic view of dense water formation and spreading at basin scale. Five months after its formation, the dense water of coastal origin created a distinct bottom layer up to a few hundreds of meters thick over the central part of the NW Mediterranean basin, which was overlaid by a layer of newly formed deep water produced by open-sea convection. These new observations highlight the role of intense episodes of both dense shelf water cascading and open-sea convection to the progressive modification of the NW Mediterranean deep waters.
Original language | English |
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Pages (from-to) | 1379-1385 |
Number of pages | 6 |
Journal | Geophysical Research Letters |
Volume | 40 |
Issue number | 7 |
Early online date | 15 Apr 2013 |
DOIs | |
Publication status | Published - 27 Apr 2013 |
Keywords
- Dense water formation
- Mediterranean Sea
- Open-sea convection
- Dense shelf water cascading