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• W2949673931 abstract "Abstract The cycling of climate into and out of glacial states in response to orbital forcing illustrates the important role of feedbacks in the Earth system. In this contribution, the Geophysical Fluid Dynamics Laboratory coupled ocean‐atmosphere model is used to qualitatively assess how changes in the Earth's precessional parameters may have impacted Atlantic Meridional Ocean Circulation and Southern Ocean dynamics. The Southern Ocean region responds to precessional forcing similar to that of the Last Glacial Maximum with a slight shift in maximum average annual wind stress, a reduction in austral winter wind stress, and an increase in austral winter sea ice. During austral summer, stratification and wind stress increase, Changes in the temperature and density of the North Atlantic lead to a decrease in Atlantic Meridional Overturning Circulation. Together these changes contribute to aging of the global deep ocean, except around Antarctica where enhanced local convection decreases the age of upwelling waters. These circulation changes may have implications for a precessionally driven feedback that contributes to enhanced storage of CO 2 in the deep ocean and a reduction in atmospheric CO 2 ." @default.
• W2949673931 created "2019-06-27" @default.
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• W2949673931 date "2019-07-01" @default.
• W2949673931 modified "2023-10-18" @default.
• W2949673931 title "Response of the High‐Latitude Southern Hemisphere to Precessional Forcing: Implications for Pleistocene Ocean Circulation" @default.
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• W2949673931 doi "https://doi.org/10.1029/2019pa003598" @default.
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