Year-to-Year Reoutcropping of Eighteen Degree Water in an Eddy-Resolving Ocean Simulation

• Published in: Journal of physical oceanography Vol. 45; no. 4; pp. 1189 - 1204
• Main Authors: Kwon, Young-Oh, Park, Jong-Jin, Gary, Stefan F., Lozier, M. Susan
• Format: Journal Article
• Language: English
• Published: Boston American Meteorological Society 01.04.2015
• Subjects: Anomalies; General circulation models; Heat; Meteorology; Ocean currents; Outcrops; Sea surface; Sea surface temperature; Sea surface temperature anomalies; Simulation; Surface temperature; Temperature anomalies; Vortices; Winter
• ISSN: 0022-3670; 1520-0485
• DOI: 10.1175/JPO-D-14-0122.1

Abstract Winter outcropping of the Eighteen Degree Water (EDW) and its subsequent dispersion are studied using a ° eddy-resolving simulation of the Family of Linked Atlantic Modeling Experiments (FLAME). Outcropped EDW columns in the model simulations are detected in each winter from 1990 to 1999, and particles are deployed in the center of each outcropped EDW column. Subsequently, the trajectories of these particles are calculated for the following 5 yr. The particles slowly spread away from the outcropping region into the nonoutcropping/subducted EDW region south of ~30°N and eventually to the non-EDW region in the greater subtropical gyre. Approximately 30% of the particles are found in non-EDW waters 1 yr after deployment; after 5 yr, only 25% of the particles are found within EDW. The reoutcropping time is defined as the number of years between when a particle is originally deployed in an outcropping EDW column and when that particle is next found in an outcropping EDW column. Of the particles, 66% are found to reoutcrop as EDW in 1 yr, and less than 5% of the particles outcrop in each of the subsequent 4 yr. While the individual trajectories exhibit significant eddy-like motions, the time scale of reoutcropping is primarily set by the mean circulation. The dominance of reoutcropping in 1 yr suggests that EDW outcropping contributes considerably to the persistence of surface temperature anomalies from one winter to the next, that is, the reemergence of winter sea surface temperature anomalies.