The type of surface radiative forcing in radiative-convective equilibrium explains the spread in global climate response across CMIP5 models

Chirag Dhara1, Maik Renner2 and Axel Kleidon1, (1)Max-Planck-Institute for Biogeochemistry, Biospheric Theory and Modelling Group, Jena, Germany, (2)Max Planck Institute for Biogeochemistry, Biospheric Theory and Modelling Group, Jena, Germany
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