Signal-to-noise ratios for the detection of ocean circulation changes


Contact
lohmann [ at ] awi-bremerhaven.de

Abstract

Our analysis shows that the temperature structure in the Atlantic Ocean can be a sensitive indicator identifying early Atlantic thermohaline circulation (THC) weakening with a high signal-to-noise ratio. Simulations with the coupled atmosphere-ocean circulation model ECHAM5/MPI-OM emphasize the subsurface temperature signature in the Atlantic Ocean with its potential to trace THC changes. A part of this signature can be understood with the advective-diffusive balance which is confirmed in a stochastic low-order model of the Atlantic Ocean circulation. It is shown that the integration of noise, which enters in a multiplicative way into the stochastic differential equation, is linked to the predictive skill of mid-depth temperatures for possible THC change.



Item Type
Conference (Talk)
Authors
Divisions
Programs
Peer revision
Not peer-reviewed
Publication Status
Published
Event Details
European Geosciences Union, 2nd General Assembly, 24-29 April 2005, Vienna, Austria..
Eprint ID
12710
Cite as
Lohmann, G. , Haak, H. , Jungclaus, J. and Prange, M. (2005): Signal-to-noise ratios for the detection of ocean circulation changes , European Geosciences Union, 2nd General Assembly, 24-29 April 2005, Vienna, Austria. .


Share

Research Platforms
N/A

Campaigns


Actions
Edit Item Edit Item