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  Mid-Pleistocene transition in glacial cycles explained by declining CO2 and regolith removal

Willeit, M., Ganopolski, A., Calov, R., Brovkin, V. (2019): Mid-Pleistocene transition in glacial cycles explained by declining CO2 and regolith removal. - Science Advances, 5, eaav7337.
https://doi.org/10.1126/sciadv.aav7337

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???ViewItemFull_lblCiteItemAs???: https://publications.pik-potsdam.de/pubman/item/item_23117 ???ViewItemFull_lblCiteItemVersionAs???: https://publications.pik-potsdam.de/pubman/item/item_23117_4
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Willeit, Matteo1, ???ENUM_CREATORROLE_AUTHOR???                 
Ganopolski, Andrey1, ???ENUM_CREATORROLE_AUTHOR???           
Calov, Reinhard1, ???ENUM_CREATORROLE_AUTHOR???           
Brovkin, V.2, ???ENUM_CREATORROLE_AUTHOR???
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1Potsdam Institute for Climate Impact Research, Potsdam, ou_persistent13              
2External Organizations, ou_persistent22              

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 ???ViewItemFull_lblAbstract???: Variations in Earth’s orbit pace the glacial-interglacial cycles of the Quaternary, but the mechanisms that transform regional and seasonal variations in solar insolation into glacial-interglacial cycles are still elusive. Here, we present transient simulations of coevolution of climate, ice sheets, and carbon cycle over the past 3 million years. We show that a gradual lowering of atmospheric CO2 and regolith removal are essential to reproduce the evolution of climate variability over the Quaternary. The long-term CO2 decrease leads to the initiation of Northern Hemisphere glaciation and an increase in the amplitude of glacial-interglacial variations, while the combined effect of CO2 decline and regolith removal controls the timing of the transition from a 41,000- to 100,000-year world. Our results suggest that the current CO2 concentration is unprecedented over the past 3 million years and that global temperature never exceeded the preindustrial value by more than 2°C during the Quaternary.

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 ???ViewItemFull_lblDates???: 2019
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 ???ViewItemFull_lblIdentifiers???: ???ENUM_IDENTIFIERTYPE_DOI???: 10.1126/sciadv.aav7337
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???ENUM_IDENTIFIERTYPE_EDOC???: 8472
???ENUM_IDENTIFIERTYPE_RESEARCHTK???: Paleoclimate
???ENUM_IDENTIFIERTYPE_RESEARCHTK???: Ice
???ENUM_IDENTIFIERTYPE_RESEARCHTK???: Atmosphere
???ENUM_IDENTIFIERTYPE_RESEARCHTK???: Oceans
???ENUM_IDENTIFIERTYPE_RESEARCHTK???: Nonlinear Dynamics
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???ENUM_IDENTIFIERTYPE_MODELMETHOD???: SICOPOLIS
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???ViewItemFull_lblSourceTitle???: Science Advances
???ViewItemFull_lblSourceGenre???: ???ENUM_GENRE_JOURNAL???, SCI, Scopus, p3, oa
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