Convection in the Greenland Sea : Model and Observations

The Meridional overturning circulation (MOC) is one crucial component in Earth's climate system, redistributing heat round the globe. The abyssal limb of the MOC is fed by the deep water formation near the poles. A basic requirement for any successful climate model simulation is the ability to...

Full description

Bibliographic Details
Main Author: Nummelin, Aleksi
Other Authors: Helsingin yliopisto, Matemaattis-luonnontieteellinen tiedekunta, Fysiikan laitos, University of Helsinki, Faculty of Science, Department of Physics, Helsingfors universitet, Matematisk-naturvetenskapliga fakulteten, Institutionen för fysik
Format: Master Thesis
Language:English
Published: Helsingfors universitet 2012
Subjects:
Online Access:http://hdl.handle.net/10138/32702