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Recent Tropical Pacific cooling and Walker circulation strengthening driven by anthropogenic emissions

Pedro
DiNezio
Department of Atmospheric and Oceanic Sciences, CU Boulder
Clara Deser, NCAR
Ping Chang, Texas A&M University
Nan Rosenbloom, NCAR
Carolina Vera, University of Buenos Aires
Nicola Maher, Australian National University
Julia Mindlin, University of Buenos Aires
Sol Osman, University of Buenos Aires
Robb Wills, ETH
Jeremy Klavans, CU Boulder
Talk
The eastern tropical Pacific Ocean has been cooling over the past forty years alongside with a strengthening of the Walker Circulation. Global climate models cannot simulate these trends confounding the causes of environmental changes globally. We address this issue with an unprecedented ensemble of high resolution global climate simulations that produce a response to human emissions explaining observed changes. This forced response is amplified by a positive feedback loop arising from interactions between the tropical Pacific and the Southern Ocean previously not active in climate models. Simulating these interactions depends on an accurate representation of the climatology of the tropical Pacific, as well as ocean mesoscale features – requiring enhanced atmospheric and oceanic resolution. The simulated response reveals a large human influence on observed changes, revising the previous consensus of a natural cause.
Presentation file