Tightened constraints on the time-lag between Antarctic temperature and CO 2 during the last deglaciation
- 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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Tightened constraints on the time-lag between Antarctic temperature and CO 2 during the last deglaciation ; volume:8 ; number:4 ; year:2012 ; pages:1213-1221
Climate of the past ; 8, Heft 4 (2012), 1213-1221
- Creator
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Pedro, J. B.
Rasmussen, S. O.
Van Ommen, T. D.
- DOI
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10.5194/cp-8-1213-2012
- URN
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urn:nbn:de:101:1-201710277887
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
- 15.08.2025, 7:34 AM CEST
Data provider
This object is provided by:
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Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Pedro, J. B.
- Rasmussen, S. O.
- Van Ommen, T. D.
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Antarctic temperature and CO 2 : near-synchrony yet variable phasing during the last deglaciation
A glacial systems model configured for large ensemble analysis of Antarctic deglaciation
The last deglaciation: timing the bipolar seesaw
Modelling firn thickness evolution during the last deglaciation: constraints on sensitivity to temperature and impurities
Climate bifurcation during the last deglaciation?
On deglaciation induced perturbations of the geoid
The new Kr-86 excess ice core proxy for synoptic activity: West Antarctic storminess possibly linked to ITCZ movement through the last deglaciation
Paleo Agulhas rings enter the subtropical gyre during the penultimate deglaciation
New age constraints reveal moraine stabilization thousands of years after deposition during the last deglaciation of western New York, USA
Arctic and Antarctic forcing of ocean interior warming during the last deglaciation
Leads and lags between Antarctic temperature and carbon dioxide during the last deglaciation
Thickness of the divide and flank of the West Antarctic Ice Sheet through the last deglaciation
Antarctic temperature and CO 2 : near-synchrony yet variable phasing during the last deglaciation
A glacial systems model configured for large ensemble analysis of Antarctic deglaciation
The last deglaciation: timing the bipolar seesaw
Modelling firn thickness evolution during the last deglaciation: constraints on sensitivity to temperature and impurities
Climate bifurcation during the last deglaciation?
On deglaciation induced perturbations of the geoid
The new Kr-86 excess ice core proxy for synoptic activity: West Antarctic storminess possibly linked to ITCZ movement through the last deglaciation
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