- Location
-
Deutsche Nationalbibliothek Frankfurt am Main
- Extent
-
Online-Ressource
- Language
-
Englisch
- Bibliographic citation
-
The middle-to-late Eocene greenhouse climate, modelled using the CESM 1.0.5 ; year:2020 ; pages:1-44
Climate of the past discussions ; (2020), 1-44
- Creator
-
Baatsen, Michiel
von der Heydt, Anna S.
Huber, Matthew
Kliphuis, Michael A.
Bijl, Peter K.
Sluijs, Appy
Dijkstra, Henk A.
- DOI
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10.5194/cp-2020-29
- URN
-
urn:nbn:de:101:1-2020031204352179524617
- Rights
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
-
14.08.2025, 11:00 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Baatsen, Michiel
- von der Heydt, Anna S.
- Huber, Matthew
- Kliphuis, Michael A.
- Bijl, Peter K.
- Sluijs, Appy
- Dijkstra, Henk A.
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Polar amplification of orbital-scale climate variability in the early Eocene greenhouse world
Vegetation change across the Drake Passage region linked to late Eocene cooling and glacial disturbance after the Eocene–Oligocene transition
Vegetation change across the Drake Passage region linked to late Eocene cooling and glacial disturbance after the Eocene–Oligocene Transition
Evolution of continental temperature seasonality from the Eocene greenhouse to the Oligocene icehouse-A model-data comparison
Evolution of continental temperature seasonality from the Eocene greenhouse to the Oligocene icehouse –a model–data comparison
Middle and late Eocene fish otoliths from the eastern and southern USA
Equilibrium state and sensitivity of the simulated middle-to-late Eocene climate
No paleoclimatic anomalies are associated with the late Eocene extraterrestrial impact events
Late Eocene onset of the Proto-Antarctic Circumpolar Current
Middle Eocene greenhouse warming facilitated by diminished weathering feedback
Dry hydroclimates in the late Palaeocene-early Eocene hothouse world
Polar amplification of orbital-scale climate variability in the early Eocene greenhouse world
Polar amplification of orbital-scale climate variability in the early Eocene greenhouse world
Vegetation change across the Drake Passage region linked to late Eocene cooling and glacial disturbance after the Eocene–Oligocene transition
Vegetation change across the Drake Passage region linked to late Eocene cooling and glacial disturbance after the Eocene–Oligocene Transition
Evolution of continental temperature seasonality from the Eocene greenhouse to the Oligocene icehouse-A model-data comparison
Evolution of continental temperature seasonality from the Eocene greenhouse to the Oligocene icehouse –a model–data comparison
Middle and late Eocene fish otoliths from the eastern and southern USA
Equilibrium state and sensitivity of the simulated middle-to-late Eocene climate
No paleoclimatic anomalies are associated with the late Eocene extraterrestrial impact events
Late Eocene onset of the Proto-Antarctic Circumpolar Current
Middle Eocene greenhouse warming facilitated by diminished weathering feedback
Dry hydroclimates in the late Palaeocene-early Eocene hothouse world
Polar amplification of orbital-scale climate variability in the early Eocene greenhouse world
Polar amplification of orbital-scale climate variability in the early Eocene greenhouse world
Vegetation change across the Drake Passage region linked to late Eocene cooling and glacial disturbance after the Eocene–Oligocene transition
Vegetation change across the Drake Passage region linked to late Eocene cooling and glacial disturbance after the Eocene–Oligocene Transition
Evolution of continental temperature seasonality from the Eocene greenhouse to the Oligocene icehouse-A model-data comparison
Evolution of continental temperature seasonality from the Eocene greenhouse to the Oligocene icehouse –a model–data comparison
Middle and late Eocene fish otoliths from the eastern and southern USA
Equilibrium state and sensitivity of the simulated middle-to-late Eocene climate