Antarctic ice sheet and oceanographic response to eccentricity forcing during the early Miocene
- Location
-
Deutsche Nationalbibliothek Frankfurt am Main
- Extent
-
Online-Ressource
- Language
-
Englisch
- Bibliographic citation
-
Antarctic ice sheet and oceanographic response to eccentricity forcing during the early Miocene ; volume:7 ; number:3 ; year:2011 ; pages:869-880
Climate of the past ; 7, Heft 3 (2011), 869-880
- Creator
-
Liebrand, D.
Lourens, L. J.
Hodell, D. A.
de Boer, B.
van de Wal, R. S. W.
Pälike, H.
- DOI
-
10.5194/cp-7-869-2011
- URN
-
urn:nbn:de:101:1-2017102714760
- Rights
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
-
15.08.2025, 7:27 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
- Liebrand, D.
- Lourens, L. J.
- Hodell, D. A.
- de Boer, B.
- van de Wal, R. S. W.
- Pälike, H.
Other Objects (12)
Antarctic ice sheet expansions in the Middle Miocene and Pliocene
Net effect of ice-sheet–atmosphere interactions reduces simulated transient Miocene Antarctic ice-sheet variability
Antarctic ice-sheet response to atmospheric CO 2 and insolation in the Middle Miocene
East Antarctic Ice Sheet Variability In The Central Transantarctic Mountains Since The Mid Miocene
Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing
Nonlinear response of the Antarctic ice sheet to Quaternary sea level and climate forcing
Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing
Competing influences of the ocean, atmosphere and solid earth on transient Miocene Antarctic ice sheet variability
Quaternary Antarctic Ice Sheet Dynamics
Miocene Antarctic Ice Sheet area adapts significantly faster than volume to CO<sub>2</sub>-induced climate change
Miocene Antarctic ice sheet area responds significantly faster than volume to CO<sub>2</sub>-induced climate change
Late Miocene onset of the modern Antarctic Circumpolar Current
Antarctic ice sheet expansions in the Middle Miocene and Pliocene
Net effect of ice-sheet–atmosphere interactions reduces simulated transient Miocene Antarctic ice-sheet variability
Antarctic ice-sheet response to atmospheric CO 2 and insolation in the Middle Miocene
East Antarctic Ice Sheet Variability In The Central Transantarctic Mountains Since The Mid Miocene
Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing
Nonlinear response of the Antarctic ice sheet to Quaternary sea level and climate forcing
Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing
Competing influences of the ocean, atmosphere and solid earth on transient Miocene Antarctic ice sheet variability
Quaternary Antarctic Ice Sheet Dynamics
Miocene Antarctic Ice Sheet area adapts significantly faster than volume to CO<sub>2</sub>-induced climate change
Miocene Antarctic ice sheet area responds significantly faster than volume to CO<sub>2</sub>-induced climate change
Late Miocene onset of the modern Antarctic Circumpolar Current
Antarctic ice sheet expansions in the Middle Miocene and Pliocene
Net effect of ice-sheet–atmosphere interactions reduces simulated transient Miocene Antarctic ice-sheet variability
Antarctic ice-sheet response to atmospheric CO 2 and insolation in the Middle Miocene
East Antarctic Ice Sheet Variability In The Central Transantarctic Mountains Since The Mid Miocene
Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing
Nonlinear response of the Antarctic ice sheet to Quaternary sea level and climate forcing
Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing
Competing influences of the ocean, atmosphere and solid earth on transient Miocene Antarctic ice sheet variability
Quaternary Antarctic Ice Sheet Dynamics
Miocene Antarctic Ice Sheet area adapts significantly faster than volume to CO<sub>2</sub>-induced climate change
Miocene Antarctic ice sheet area responds significantly faster than volume to CO<sub>2</sub>-induced climate change