Impact of slowdown of Atlantic overturning circulation on heat and freshwater transports. Issue 14 (25th July 2016)

• Record Type: Journal Article
• Authors: Kelly, Kathryn A.; Drushka, Kyla; Thompson, LuAnne; Le Bars, Dewi; McDonagh, Elaine L.
• Is Part Of: Geophysical research letters. Volume 43:Issue 14(2016)
• Page Start: 7625
• Page End: 7631
• Publication Date: 2016-07-25
• Subjects: AMOC -- heat transport -- freshwater; Geophysics -- Periodicals; Planets -- Periodicals; Lunar geology -- Periodicals; 550
• DOI: 10.1002/2016GL069789
• Languages: English
• ISSNs: 0094-8276

Abstract

Abstract: Recent measurements of the strength of the Atlantic overturning circulation at 26°N show a 1 year drop and partial recovery amid a gradual weakening. To examine the extent and impact of the slowdown on basin wide heat and freshwater transports for 2004–2012, a box model that assimilates hydrographic and satellite observations is used to estimate heat transport and freshwater convergence as residuals of the heat and freshwater budgets. Using an independent transport estimate, convergences are converted to transports, which show a high level of spatial coherence. The similarity between Atlantic heat transport and the Agulhas Leakage suggests that it is the source of the surface heat transport anomalies. The freshwater budget in the North Atlantic is dominated by a decrease in freshwater flux. The increasing salinity during the slowdown supports modeling studies that show that heat, not freshwater, drives trends in the overturning circulation in a warming climate. Key Points: Overturning slowdown decreases heat and freshwater transport Agulhas Leakage is likely source of decreased heat transport Freshwater convergence is not causing AMOC slowdown