Water mass transformations in the Mediterranean outflow water

The start of the Atlantic Meridional Overturning Circulation takes place at high latitudes in the North Atlantic Ocean, through the deep convection of surface waters. For these surface waters to reach the deep ocean it is necessary that the upper and intermediate waters be sufficiently salty, i.e. p...

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Bibliographic Details
Main Authors: Gasser, Marc, Pelegrí Llopart, Josep Luis, Bruno, Miguel, Chioua, Jamal, Emelianov, Mikhail, Machín Jiménez, Francisco José, Rodríguez Santana, Ángel
Other Authors: BU-BAS
Format: Conference Object
Language:English
Published: 2014
Subjects:
Online Access:http://hdl.handle.net/10553/114717