A Southern Ocean mode of multidecadal variability. Issue 5 (7th March 2016)

• Record Type: Journal Article
• Authors: Le Bars, D.; Viebahn, J. P.; Dijkstra, H. A.
• Is Part Of: Geophysical research letters. Volume 43:Issue 5(2016)
• Page Start: 2102
• Page End: 2110
• Publication Date: 2016-03-07
• Subjects: multidecadal variability -- intrinsic variability -- baroclinic instability -- Southern Ocean -- mode of variability -- ocean heat content; Geophysics -- Periodicals; Planets -- Periodicals; Lunar geology -- Periodicals; 550
• DOI: 10.1002/2016GL068177
• Languages: English
• ISSNs: 0094-8276

Abstract

Abstract: A 250 year simulation of a strongly eddying global version of the Parallel Ocean Program (POP) model reveals a new mode of intrinsic multidecadal variability, the Southern Ocean Mode (SOM), with a period of 40–50 year. The peak‐to‐peak difference in the global ocean heat content within a multidecadal cycle is up to 60 ZJ. This change results from surface heat flux variations in the South Atlantic and propagation of temperature anomalies along the Antarctic Circumpolar Current and into the Weddell gyre around 30°E. The temperature anomalies propagate as deep as 5000 m along the isopycnals between 50°S and 30°S and induce multidecadal changes in the Atlantic Meridional Overturning Circulation. A positive feedback loop between the generation of eddies through baroclinic instability and the dynamics of the mean circulation is essential for the existence of the SOM. The dominant physics appears similar to that responsible for variability found in a three‐layer quasi‐geostrophic eddy‐resolving model. This combined with the fact that the SOM is not found in a noneddying version of the same global POP model further suggests that eddy processes are crucial for its existence and/or excitation. Key Points: A new mode of internal ocean variability is identified in the Southern Ocean It has an important impact on global ocean heat uptake It depends on baroclinic instabilities from mesoscale eddies in the Antarctic Circumpolar Current