Multiple ocean equilibria and decoupling of Miocene atmospheric pCO2 and regional temperatures

Résumé fourni par la source

During the Middle Miocene Climate Transition (MMCT; ~14.7–13.8 Ma), the global climate experienced rapid cooling, leading to modern-like temperatures, precipitation patterns, and permanent ice sheets. However, proxy records indicate that atmospheric pCO2 and regional climate conditions (SST, ice volume) were highly variable from 17 to 12.5 Ma and these changes were not always synchronous. Here, we report on a series of middle Miocene simulations using the water isotope enabled earth system model (iCESM1.2) to explore the potential for multiple equilibrium states to explain the observed decoupling between pCO2 and regional climates. Our simulations indicate that initial ocean conditions can significantly influence deep water formation in the North Atlantic and lead to multiple ocean equilibria. When the model is initiated from a cold state, residual cool surface water temperatures in the North Atlantic intensify Atlantic Meridional Ocean Circulation (AMOC) and inhibit Arctic sea-ice formation. When initiated from a warm state, the AMOC remains weak. The different ocean states drive differences in equator-to-pole sea surface temperature gradients and sea ice distributions through heat redistribution changes. These equilibria cause variations in temperature gradients and sea ice distribution due to changes in heat redistribution. Additionally, changes in ocean circulation and a reduced temperature gradient in the North Atlantic increase North Atlantic precipitation when the AMOC is strong. These findings underscore the importance of the ocean’s initial state in shaping regional climate responses to atmospheric pCO2, potentially explaining regional climate pattern variability observed during the Miocene.

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