An analogue model to derive additional climate change scenarios from existing GCM simulations

By C. Huntingford, P. Cox. 2000

161 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/7275808ac26841d58517fd99f339d63efa8991d9

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

1. J. Gregory
2. M. Webb
3. Jouni Raäisaänen
4. Alexander J. Krause
5. M. Joshi
6. M. Byrne
7. T. Lenton
8. D. Hill

In Global and Planetary Change

1. J. Gregory
2. M. Webb
3. Jouni Raäisaänen
4. T. Lenton
5. Lindsey J Atkinson
6. R. Fisher
7. F. Woodward
8. J. Zaragoza‐Castells

Citations in the corpus

• Modelling the long-term carbon cycle, atmospheric CO2, and Earth surface temperature from late Neoproterozoic to present day (2019, background): “More economically, if for a given paleogeography it can be established from the climatemodel that the spatial pattern of precipitation changes scales with global average temperature – as is the case for the modern climate – then a pattern-scaling approach can be taken (Huntingford et al., 2010; Hunt”
• Using temperature‐dependent changes in leaf scaling relationships to quantitatively account for thermal acclimation of respiration in a coupled global climate–vegetation model (2008, methodology): “JULES was driven globally within the IMOGEN land surface model (Huntingford & Cox, 2000).”
• How reliable are climate models? (2007, background): “First, model simulations suggest that the magnitude of regional climate changes increases quasi-linearly with the change in global mean temperature (e.g. Santer et al., 1990; Mitchell et al., 1999; Huntingford and Cox, 2000; Mitchell, 2003; Harvey, 2004), at least for forcing scenarios dominated by ”
• Land–Ocean Warming Contrast over a Wide Range of Climates: Convective Quasi-Equilibrium Theory and Idealized Simulations (2013, background): “Lambert and Chiang (2007) extend the energy approach by including a land–ocean heat flux, which helps to maintain the relatively constant amplification factor that is a feature of observations and simulations (Huntingford and Cox 2000; Sutton et al. 2007).”
• Mechanisms for the land/sea warming contrast exhibited by simulations of climate change (2008, background): “However, the land/sea contrast is evident at most latitudes (Huntingford and Cox 2000; Cubasch et al. 2001, Fig. 14.10; Sutton et al. 2007), suggesting that a more widespread mechanism may be involved.”