Climate variability, heat distribution, and polar amplification in the warm unipolar “icehouse” of the Oligocene
Abstract ∼ 60 –90°), especially in the Southern Hemisphere (SH). Vegetation-based precipitation reconstructions of the Oligocene suggest regionally drier conditions compared to modern times around the Equator. When compared to proxy data, climate model simulations overestimate Oligocene precipitation in most areas, particularly the tropics. Temperatures around the mid- to high latitudes are generally underestimated in models compared to proxy data and tend to overestimate the warming in the tropics. In line with previous proxy-to-model comparisons, we find that models underestimate polar amplification and overestimate the Equator-to-pole temperature gradient suggested from the available proxy data. This further stresses the urgency of solving this widely recorded problem for past warm climates, such as the Oligocene.
- 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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Climate variability, heat distribution, and polar amplification in the warm unipolar “icehouse” of the Oligocene ; volume:20 ; number:7 ; year:2024 ; pages:1627-1657 ; extent:31
Climate of the past ; 20, Heft 7 (2024), 1627-1657 (gesamt 31)
- Creator
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Jenny, Dominique K. L. L.
Reichgelt, Tammo
O'Brien, Charlotte L.
Liu, Xiaoqing
Bijl, Peter K.
Huber, Matthew
Sluijs, Appy
- DOI
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10.5194/cp-20-1627-2024
- URN
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urn:nbn:de:101:1-2408061446592.418554269933
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 11:02 AM CEST
Data provider
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Jenny, Dominique K. L. L.
- Reichgelt, Tammo
- O'Brien, Charlotte L.
- Liu, Xiaoqing
- Bijl, Peter K.
- Huber, Matthew
- Sluijs, Appy