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
Deutsche Nationalbibliothek Frankfurt am Main
Extent
Online-Ressource
Language
Englisch

Bibliographic citation
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
Toumoulin, Agathe
Tardif, Delphine
Donnadieu, Yannick
Licht, Alexis
Ladant, Jean-Baptiste
Kunzmann, Lutz
Dupont-Nivet, Guillaume

DOI
10.5194/cp-18-341-2022
URN
urn:nbn:de:101:1-2022030304222791608364
Rights
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
Last update
15.08.2025, 7:24 AM CEST

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Associated

  • Toumoulin, Agathe
  • Tardif, Delphine
  • Donnadieu, Yannick
  • Licht, Alexis
  • Ladant, Jean-Baptiste
  • Kunzmann, Lutz
  • Dupont-Nivet, Guillaume

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