Climate model sensitivity to atmospheric CO2 levels in the Early–Middle Paleogene

By C. Shellito, L. Sloan, Matthew Huber. 2003

150 citations recorded by the source corpus.

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

View Paper: https://www.semanticscholar.org/paper/c2953db3ee3896e60ab530f7e5ef658ca1b81da0

How researchers see this paper

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In Atmospheric Science

1. Dorian S. Abbot
2. David R. Greenwood
3. W. Bossert
4. Eli Tziperman
5. S. B. Archibald
6. Brian D. Farrell

In Environmental Chemistry

1. Dorian S. Abbot
2. Eli Tziperman

In Global and Planetary Change

1. Dorian S. Abbot
2. Eli Tziperman

Citations in the corpus

• Seasonality, the latitudinal gradient of diversity, and Eocene insects (2010, background): “…of their seeds and seedlings to frost restricts palms to regions with CMMT .5uC; but this sensitivity increases to .8uC under conditions of elevated CO2 as are inferred for the Eocene (Sakai and Larcher, 1987; Greenwood and Wing 1995; Royer et al. 2002; Shellito et al. 2003; Sluijs et al. 2009).”
• A high‐latitude convective cloud feedback and equable climates (2008, methodology): “…circulation models (GCMs), whether coupled to a mixed-layer ocean (Sloan and Rea, 1995; Otto-Bliesner and Upchurch, 1997; Upchurch et al., 1998; Shellito et al., 2003) or to a full ocean GCM (Bush and Philander, 1997; Huber and Sloan, 2001) have consistently yielded the important result that…”