IMIS | Flanders Marine Institute
 

Flanders Marine Institute

Platform for marine research

IMIS

Publications | Institutes | Persons | Datasets | Projects | Maps
[ report an error in this record ]basket (0): add | show Printer-friendly version

A minimal model for wind- and mixing-driven overturning: threshold behavior for both driving mechanisms
Fürst, J.; Levermann, A. (2012). A minimal model for wind- and mixing-driven overturning: threshold behavior for both driving mechanisms. Clim. Dyn. 38(1-2): 239-260. dx.doi.org/10.1007/s00382-011-1003-7
In: Climate Dynamics. Springer: Berlin; Heidelberg. ISSN 0930-7575, more
Peer reviewed article  

Available in Authors 

Keyword
    Marine
Author keywords
    Meridional overturning circulation; Northern sinking; Criticalfreshwater threshold; Overturning sensitivity; Conceptual model;Stability; Atlantic meridional overturning circulation; Pycnoclinedepth; Driving mechanism

Authors  Top 
  • Fürst, J., more
  • Levermann, A.

Abstract
    We present a minimal conceptual model for the Atlantic meridional overturning circulation which incorporates the advection of salinity and the basic dynamics of the oceanic pycnocline. Four tracer transport processes following Gnanadesikan in Science 283(5410):2077-2079, (1999) allow for a dynamical adjustment of the oceanic pycnocline which defines the vertical extent of a mid-latitudinal box. At the same time the model captures the salt-advection feedback (Stommel in Tellus 13(2):224-230, (1961)). Due to its simplicity the model can be solved analytically in the purely wind- and purely mixing-driven cases. We find the possibility of abrupt transition in response to surface freshwater forcing in both cases even though the circulations are very different in physics and geometry. This analytical approach also provides expressions for the critical freshwater input marking the change in the dynamics of the system. Our analysis shows that including the pycnocline dynamics in a salt-advection model causes a decrease in the freshwater sensitivity of its northern sinking up to a threshold at which the circulation breaks down. Compared to previous studies the model is restricted to the essential ingredients. Still, it exhibits a rich behavior which reaches beyond the scope of this study and might be used as a paradigm for the qualitative behaviour of the Atlantic overturning in the discussion of driving mechanisms.

All data in IMIS is subject to the VLIZ privacy policy Top | Authors