The effect of a localized geothermal heat source on deep water formation

In a simplified two-dimensional model of a buoyancy-driven overturning circulation, we numerically study the response of the flow to a small localized heat source at the bottom. The flow is driven by differential thermal forcing applied along the top surface boundary. We evaluate the steady state so...

Full description

Bibliographic Details
Main Authors: M. Vincze, A. Várai, E. Barsy, I. M. Jánosi
Format: Article
Language:English
Published: Copernicus Publications 2011-11-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/18/841/2011/npg-18-841-2011.pdf