Vertical mixing estimates along hydrological sections en Atlantique Nord in North Atlantic

Vertical mixing in the ocean contributes to sustain the Meridionnal Overturning. Circulation (MOC) by allowing the renewal of deep waters. A section across the MOC is performed by the hydrological radial OVIDE repeated every two years between Portugal and Greenland since 2002. The energy required fo...

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Bibliographic Details
Main Author: Kokoszka, Florian
Other Authors: Laboratoire de physique des océans (LPO), Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS), Université de Bretagne occidentale - Brest, Herlé Mercier, Bruno Ferron
Format: Doctoral or Postdoctoral Thesis
Language:French
Published: HAL CCSD 2012
Subjects:
North Atlantic
Hydrological Section
Data Analysis
InternalWaves
Thorpe Scales
Garrett and Munk Model
Turbulence
Vertical Mixing
Dissipation
Fine-structure
Micro-structure
Parameterizations
Topography
Atantique Nord
Section Hydrologique
Analyse de données
Ondes Internes
Echelles de Thorpe
Modèle de Garrett et Munk
Mélange vertical
Finestructure
Microstructure
Paramétrisations
Topographie
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Greenland
Mid-Atlantic Ridge
Munk
Online Access:https://theses.hal.science/tel-02071038
https://theses.hal.science/tel-02071038/document
https://theses.hal.science/tel-02071038/file/These-2012-EDSM-Oceanographie_physique-KOKOSZKA_Florian.pdf

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