Response of a comprehensive climate model to a broad range of external forcings : relevance for deep ocean ventilation and the development of late Cenozoic ice ages

• Published in: Climate Dynamics
• Main Authors: Galbraith, Eric, de Lavergne, C.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2019
• Subjects: Ocean circulation; Climate; Earth system model; Carbon dioxide; Ice ages; Ocean biogeochemistry; Antarctic; Southern Ocean; The Antarctic; Antarc*; Ice Sheet; NADW; North Atlantic; Sea ice
• Online Access: https://ddd.uab.cat/record/223796

Unidad de excelencia María de Maeztu MdM-2015-0552 Over the past few million years, the Earth descended from the relatively warm and stable climate of the Pliocene into the increasingly dramatic ice age cycles of the Pleistocene. The influences of orbital forcing and atmospheric CO on land-based ice sheets have long been considered as the key drivers of the ice ages, but less attention has been paid to their direct influences on the circulation of the deep ocean. Here we provide a broad view on the influences of CO , orbital forcing and ice sheet size according to a comprehensive Earth system model, by integrating the model to equilibrium under 40 different combinations of the three external forcings. We find that the volume contribution of Antarctic (AABW) vs. North Atlantic (NADW) waters to the deep ocean varies widely among the simulations, and can be predicted from the difference between the surface densities at AABW and NADW deep water formation sites. Minima of both the AABW-NADW density difference and the AABW volume occur near interglacial CO (270-400 ppm). At low CO , abundant formation and northward export of sea ice in the Southern Ocean contributes to very salty and dense Antarctic waters that dominate the global deep ocean. Furthermore, when the Earth is cold, low obliquity (i.e. a reduced tilt of Earth's rotational axis) enhances the Antarctic water volume by expanding sea ice further. At high CO , AABW dominance is favoured due to relatively warm subpolar North Atlantic waters, with more dependence on precession. Meanwhile, a large Laurentide ice sheet steers atmospheric circulation as to strengthen the Atlantic Meridional Overturning Circulation, but cools the Southern Ocean remotely, enhancing Antarctic sea ice export and leading to very salty and expanded AABW. Together, these results suggest that a 'sweet spot' of low CO , low obliquity and relatively small ice sheets would have poised the AMOC for interruption, promoting Dansgaard-Oeschger-type abrupt change. The deep ocean temperature and ...