Climate Change Projections for the Twenty-First Century and Climate Change Commitment in the CCSM3

By Gerald A. Meehl, Warren M. Washington, Benjamin D. Santer, William D. Collins, J. Arblaster, Aixue Hu, D. Lawrence, H. Teng, L. Buja, W. Strand. 2006

275 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/abf9f1364edb148c978ecbdb08a76cf4144185cf

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

In Global and Planetary Change

Citations in the corpus

Effects of long-term climate change on global building energy expenditures (2018, methodology): “…uses spatially explicit gridded temperature profiles from the Community Earth SystemModel (CESM) run fulfilling the RCP 4.5 concentration pathway, and the 8.5 Climate Scenario uses the same information from the CESMmodel run fulfilling the RCP 8.5 concentration pathway (Meehl et al., 2006).”
Stability of tallgrass prairie during a 19‐year increase in growing season precipitation (2012, background): “Although North American tallgrass prairie evolved with fire (Axelrod 1985), other manipulations (N addition) have produced rapid shifts in species composition and abundance in frequently burned prairie (Vinton et al. 1993; Hartnett, Hickman & Walter 1996).”
Climate System Response to External Forcings and Climate Change Projections in CCSM4 (2012, methodology): “This issue was also weakly pre-sent in the CCSM3 SLP projections (Meehl et al. 2006) but presumably the higher climate sensitivity of the CCSM4 has led to its ampliﬁcation in the RCP scenario simulations.”
Future climate change in the Southern Hemisphere: Competing effects of ozone and greenhouse gases (2011, methodology): “While GHGs are the dominant forcing by the end of the 21st Century, ozone forcing in the simulations likely 4 of 6 biases their result, resulting in a stronger influence of lower polar stratospheric cooling than that indicated by Figure 3d (while slightly different methodologies between our studies ”
Two Limits of Initial-Value Decadal Predictability in a CGCM (2010, methodology): “Meehl et al. (2006b) point out that ENSO variability weakens in CCSM3 in reaction to increased GHG concentrations, and in results not shown here we have found that even larger changes in variability in our A1B experiment occur in the North Atlantic near the end of the integrations.”
Centennial-scale climate change from decadally-paced explosive volcanism: a coupled sea ice-ocean mechanism (2011, methodology): “CCSM has been used extensively for paleoclimate studies (e.g., Otto-Bliesner et al. 2006a, b; Liu et al. 2009; Kaufman et al. 2009) as well as twentieth and twenty-first century simulations (e.g., Meehl et al. 2006; Holland et al. 2006a).”
The influence of anthropogenic aerosol on multi-decadal variations of historical global climate (2013, background): “C1 anthropogenic concentrations are the (Meehl et al 2006) a The difference between the historical simulation and a historical simulation with anthropogenic aerosol ﬁxed at 1860 levels.”