Forcing of anthropogenic aerosols on temperature trends of the sub-thermocline southern Indian Ocean3

• Published in: Scientific Reports
• Main Authors: Cowan, T, Cai, W, Purich, A, Rotstayn, L, England, MH
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Nature 2013
• Subjects: 37 Earth Sciences; 3708 Oceanography; 3701 Atmospheric Sciences; 13 Climate Action; anzsrc-for: 37 Earth Sciences; anzsrc-for: 3708 Oceanography; anzsrc-for: 3701 Atmospheric Sciences; Indian; North Atlantic
• Online Access: http://hdl.handle.net/1959.4/unsworks_42116; https://unsworks.unsw.edu.au/bitstreams/681ae4a8-5170-4033-8964-5673f568328b/download; https://doi.org/10.1038/srep02245

In the late twentieth century, the sub-thermocline waters of the southern tropical and subtropical Indian Ocean experienced a sharp cooling. This cooling has been previously attributed to an anthropogenic aerosol-induced strengthening of the global ocean conveyor, which transfers heat from the subtropical gyre latitudes toward the North Atlantic. From the mid-1990s the sub-thermocline southern Indian Ocean experienced a rapid temperature trend reversal. Here we show, using climate models from phase 5 of the Coupled Model Intercomparison Project, that the late twentieth century sub-thermocline cooling of the southern Indian Ocean was primarily driven by increasing anthropogenic aerosols and greenhouse gases. The models simulate a slow-down in the sub-thermocline cooling followed by a rapid warming towards the mid twenty-first century. The simulated evolution of the Indian Ocean temperature trend is linked with the peak in aerosols and their subsequent decline in the twenty-first century, reinforcing the hypothesis that aerosols influence ocean circulation trends.