Constraint of the CO2 rise by new atmospheric carbon isotopic measurements during the last deglaciation
Open Access
- 17 June 2010
- journal article
- research article
- Published by American Geophysical Union (AGU) in Global Biogeochemical Cycles
- Vol. 24 (2)
- https://doi.org/10.1029/2009gb003545
Abstract
No abstract availableKeywords
This publication has 91 references indexed in Scilit:
- Change in CO2 concentration and O2/N2 ratio in ice cores due to molecular diffusionGeophysical Research Letters, 2009
- Oceanic sources, sinks, and transport of atmospheric CO2Global Biogeochemical Cycles, 2009
- Rates of change in natural and anthropogenic radiative forcing over the past 20,000 yearsProceedings of the National Academy of Sciences, 2008
- Evidence from the high‐latitude North Atlantic for variations in Antarctic Intermediate water flow during the last deglaciationGeochemistry, Geophysics, Geosystems, 2005
- The attenuation of fast atmospheric CH4 variations recorded in polar ice coresGeophysical Research Letters, 2003
- Pleistocene vertical carbon isotope and carbonate gradients in the South Atlantic sector of the Southern OceanGeochemistry, Geophysics, Geosystems, 2003
- Hemispheric roles of climate forcings during glacial‐interglacial transitions as deduced from the Vostok record and LLN‐2D model experimentsJournal of Geophysical Research: Solid Earth, 2001
- Modeling ocean–atmosphere carbon budgets during the Last Glacial Maximum–Heinrich 1 meltwater event–Bølling transitionInternational Journal of Earth Sciences, 2000
- What caused the glacial/interglacial atmospheric pCO2 cycles?Reviews of Geophysics, 2000
- Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulationPaleoceanography and Paleoclimatology, 1988