Atmospheric CO2 concentrations over the last glacial termination.

By É. Monnin, A. Indermühle, A. Dällenbach, J. Flückiger, B. Stauffer, T. Stocker, D. Raynaud, J. Barnola. Science, 2001

1,295 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Chemistry, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/ae6f52b7db069a2aa9c72589e1ad164d5c4721b4

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In Atmospheric Science

1. A. Timmermann
2. A. Mouchet
3. L. Menviel
4. O. Timm
5. Reto Knutti
6. F. Joos
7. S. Tyteca
8. E. Brady

In Environmental Chemistry

1. S. Tyteca
2. E. Brady
3. B. Otto‐Bliesner
4. D. Salas-Mélia
5. F. Joos
6. J. Blois
7. Gerrit Lohmann
8. G. Ramstein

In Global and Planetary Change

1. M. Fitzpatrick
2. A. Timmermann
3. A. Mouchet
4. L. Menviel
5. O. Timm
6. F. Joos
7. S. Tyteca
8. V. Masson‐Delmotte

Citations in the corpus

• Last Glacial Maximum and Holocene Climate in CCSM3 (2006, methodology): “Concentrations of the atmospheric greenhouse gases in the CCSM3 simulations are based on ice core measurements (Fluckiger et al. 1999; Dallenbach et al. 2000; Monnin et al. 2001 ) and differ in the PI, LGM, and mid-Holocene simulations (Table 1). Atmospheric aerosols are set at their preindustrial ”
• Space can substitute for time in predicting climate-change effects on biodiversity (2013, methodology): “CO2 data were drawn from EPICA Dome C (42), an 800,000-y composite CO2 record from East Antarctica on which the CO2 data for 22–0 kyBP are based (46).”
• Northern hemisphere storm tracks during the last glacial maximum in the PMIP2 ocean-atmosphere coupled models: energetic study, seasonal cycle, precipitation (2009, methodology): “A more detailed and quantitative analysis of model/data comparison would be of interest, especially using new pollen-based reconstructions taking the CO2 effect into account (Wu et al. 2007).”
• Feedback between deglaciation, volcanism, and atmospheric CO2 (2009, background): “The model estimate of the time history of atmospheric CO2 can be compared with atmospheric CO2 observations obtained from the Dome C (Monnin et al., 2001) and Taylor Dome (Indermühle et al.”
• What caused Earths temperature variations during the last 800,000 years? Data-based evidences on radiative forcing and constraints on climate sensitivity (2009, methodology): “…are measured with a mean temporal resolution better than 1 kyr in ice cores over the last 800 kyr, but N2O exhibits large time windows with no or biased data sets (Petit et al., 1999; Monnin et al., 2001; Siegenthaler et al., 2005; Spahni et al., 2005; Loulergue et al., 2008; Lüthi et al., 2008).”