Climate Dynamics

, Volume 24, Issue 4, pp 347–354

Dynamic sea level changes following changes in the thermohaline circulation

Authors

    • Potsdam Institute for Climate Impact Research
  • Alexa Griesel
    • Potsdam Institute for Climate Impact Research
  • Matthias Hofmann
    • Potsdam Institute for Climate Impact Research
  • Marisa Montoya
    • Facultad de Ciencias FisicasUniversidad Complutense de Madrid
  • Stefan Rahmstorf
    • Potsdam Institute for Climate Impact Research
Article

DOI: 10.1007/s00382-004-0505-y

Cite this article as:
Levermann, A., Griesel, A., Hofmann, M. et al. Clim Dyn (2005) 24: 347. doi:10.1007/s00382-004-0505-y

Abstract

Using the coupled climate model CLIMBER-3α, we investigate changes in sea surface elevation due to a weakening of the thermohaline circulation (THC). In addition to a global sea level rise due to a warming of the deep sea, this leads to a regional dynamic sea level change which follows quasi-instantaneously any change in the ocean circulation. We show that the magnitude of this dynamic effect can locally reach up to ~1 m, depending on the initial THC strength. In some regions the rate of change can be up to 20–25 mm/yr. The emerging patterns are discussed with respect to the oceanic circulation changes. Most prominent is a south-north gradient reflecting the changes in geostrophic surface currents. Our results suggest that an analysis of observed sea level change patterns could be useful for monitoring the THC strength.

Copyright information

© Springer-Verlag 2005