Investigating the impact of reemerging sea surface temperature anomalies on the winter atmospheric circulation over the North Atlantic

• Published in: Journal of Climate
• Other Authors: Cassou, Christophe (author), Deser, Clara (author), Alexander, Michael (author)
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2007
• Subjects: North Atlantic; Sea ice
• Online Access: http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-004-341; https://doi.org/10.1175/JCLI4202.1

Extratropical SSTs can be influenced by the reemergence mechanism, whereby thermal anomalies in deep winter mixed layer persist at depth through summer and are then reentrained into the mixed layer in the following winter. The impact of reemergence in the North Atlantic Ocean (NAO) upon the climate system is investigated using an atmospheric general circulation model coupled to a mixed layer ocean/ thermodynamic sea ice model.', The dominant pattern of thermal anomalies below the mixed layer in summer in a 150-yr control integration is associated with the North Atlantic SST tripole forced by the NAO in the previous winter as indicated by singular value decomposition (SVD). To isolate the reemerging signal, two additional 60-member ensemble experiments were conducted in which temperature anomalies below 40 m obtained from the SVD analysis are added to or subtracted from the control integration. The reemerging signal, given by the mean difference between the two 60-member ensembles, causes the SST anomaly tripole to recur, beginning in fall, amplifying through January, and persisting through the following spring. The atmospheric response to these SST anomalies resembles the circulation that created them the previous winter but with reduced amplitude (10-20 m at 500 mb per degrees C), modestly enhancing the winter-to-winter persistence of the NAO. Changes in the transient eddies and their interactions with the mean flow contribute to the large-scale equivalent barotropic response throughout the troposphere. The latter can also be attributed to the change in occurrence of intrinsic weather regimes.