Robust increase in equilibrium climate sensitivity under global warming
By Katharina Meraner, T. Mauritsen, Aiko Voigt. 2013
145 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/3ea6b57e7849f2d878eee5d1b05f3a25527fd01a
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
- Stephen A. Klein
- M. Zelinka
- M. Webb
- Bjorn Stevens
- Robert Pincus
- Sandrine Bony
- T. Andrews
- Piers M. Forster
In Global and Planetary Change
- Stephen A. Klein
- M. Zelinka
- M. Webb
- Bjorn Stevens
- Robert Pincus
- Sandrine Bony
- T. Andrews
- Piers M. Forster
Citations in the corpus
- The Cloud Feedback Model Intercomparison Project (CFMIP) contribution to CMIP6. (2016, background): “Significant nonlinearity has also been found in global- and regional-scale warming (e.g. Colman and McAvaney, 2009; Jonko et al., 2013; Good et al., 2015; Meraner et al., 2013) and ocean heat uptake (Bouttes et al., 2015).”
- Developments in the MPI‐M Earth System Model version 1.2 (MPI‐ESM1.2) and Its Response to Increasing CO2 (2019, background): “This was indeed the case for a series of errors in earlier versions of MPI-ESM, and it was feared that previously identified non-linearities (Heinemann et al., 2009; Meraner et al., 2013) were merely artifacts of coding errors, which we shall investigate at the end of this study.”
- Recommendations for diagnosing effective radiative forcing from climate models for CMIP6 (2016, background): “This is due to nonlinearity in the relationship between TOA irradiance and surface temperature change and has been seen before for individual models and forcings [Andrews et al., 2015;Meraner et al., 2013].”
- Causes of Higher Climate Sensitivity in CMIP6 Models (2020, background): “In many simulations, 𝜆 weakens as global temperature increases owing to evolving surface warming patterns (Andrews et al., 2015; Armour et al., 2013; Ceppi & Gregory, 2017) and to state-dependence in feedbacks (Bloch-Johnson et al., 2015; Meraner et al., 2013).”
- The Dependence of Radiative Forcing and Feedback on Evolving Patterns of Surface Temperature Change in Climate Models (2015, unknown): “fined by Murphy (1995) and Senior and Mitchell (2000), whofirst estimateda byassumingF: that is,a5 (N2 F)/DT.”