Carbon dioxide induced stomatal closure increases radiative forcing of climate via a rapid reduction in low cloudDoutriaux-Boucher, M., Webb, M. J., Gregory, J. M. ORCID: https://orcid.org/0000-0003-1296-8644 and Boucher, O. (2009) Carbon dioxide induced stomatal closure increases radiative forcing of climate via a rapid reduction in low cloud. Geophysical Research Letters, 36. L02703. 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: 10.1029/2008GL036273 Abstract/SummaryWe performed an ensemble of twelve five-year experiments using a coupled climate-carbon-cycle model with scenarios of prescribed atmospheric carbon dioxide concentration; CO2 was instantaneously doubled or quadrupled at the start of the experiments. Within these five years, climate feedback is not significantly influenced by the effects of climate change on the carbon system. However, rapid changes take place, within much less than a year, due to the physiological effect of CO2 on plant stomatal conductance, leading to adjustment in the shortwave cloud radiative effect over land, due to a reduction in low cloud cover. This causes a 10% enhancement to the radiative forcing due to CO2, which leads to an increase in the equilibrium warming of 0.4 and 0.7 K for doubling and quadrupling. The implications for calibration of energy-balance models are discussed.
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