Sensitivity of an Earth system climate model to idealized radiative forcingAndrews, T., Ringer, M. A., Doutriaux-Boucher, M., Webb, M. J. and Collins, W. J. ORCID: https://orcid.org/0000-0002-7419-0850 (2012) Sensitivity of an Earth system climate model to idealized radiative forcing. Geophysical Research Letters, 39 (10). L10702. ISSN 0094-8276 Full text not archived in this repository. It is advisable to refer to the publisher's version if you intend to cite from this work. See Guidance on citing. To link to this item DOI: 10.1029/2012gl051942 Abstract/SummaryWe diagnose forcing and climate feedbacks in benchmark sensitivity experiments with the new Met Office Hadley Centre Earth system climate model HadGEM2-ES. To identify the impact of newly-included biogeophysical and chemical processes, results are compared to a parallel set of experiments performed with these processes switched off, and different couplings with the biogeochemistry. In abrupt carbon dioxide quadrupling experiments we find that the inclusion of these processes does not alter the global climate sensitivity of the model. However, when the change in carbon dioxide is uncoupled from the vegetation, or when the model is forced with a non-carbon dioxide forcing – an increase in solar constant – new feedbacks emerge that make the climate system less sensitive to external perturbations. We identify a strong negative dust-vegetation feedback on climate change that is small in standard carbon dioxide sensitivity experiments due to the physiological/fertilization effects of carbon dioxide on plants in this model.
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