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
Deutsche Nationalbibliothek Frankfurt am Main
Extent
Online-Ressource
Language
Englisch

Bibliographic citation
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
Jenny, Dominique K. L. L.
Reichgelt, Tammo
O'Brien, Charlotte L.
Liu, Xiaoqing
Bijl, Peter K.
Huber, Matthew
Sluijs, Appy

DOI
10.5194/cp-20-1627-2024
URN
urn:nbn:de:101:1-2408061446592.418554269933
Rights
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
Last update
14.08.2025, 11:02 AM CEST

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