Evolution of continental temperature seasonality from the Eocene greenhouse to the Oligocene icehouse –a model–data comparison
Abstract p CO 2 p CO 2 p CO 2 p CO 2 ∘ C MATR increase) due to sea-ice and surface albedo feedback. Conversely, the onset of the AIS is responsible for a more constant surface albedo yearly, which leads to a strong decrease in seasonality in the southern midlatitudes to high latitudes (> 40 ∘ Δ Δ MATR patterns we reconstruct are generally consistent with the variability of the EOT biotic crisis intensity across the Northern Hemisphere and provide insights on their underlying mechanisms.
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Evolution of continental temperature seasonality from the Eocene greenhouse to the Oligocene icehouse –a model–data comparison ; volume:18 ; number:2 ; year:2022 ; pages:341-362 ; extent:22
Climate of the past ; 18, Heft 2 (2022), 341-362 (gesamt 22)
- Creator
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Toumoulin, Agathe
Tardif, Delphine
Donnadieu, Yannick
Licht, Alexis
Ladant, Jean-Baptiste
Kunzmann, Lutz
Dupont-Nivet, Guillaume
- DOI
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10.5194/cp-18-341-2022
- URN
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urn:nbn:de:101:1-2022030304222791608364
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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15.08.2025, 7:24 AM CEST
Data provider
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Toumoulin, Agathe
- Tardif, Delphine
- Donnadieu, Yannick
- Licht, Alexis
- Ladant, Jean-Baptiste
- Kunzmann, Lutz
- Dupont-Nivet, Guillaume