Stratospheric water vapour and high climate sensitivity in a version of the HadSM3 climate model
1NCAS Climate, University of Reading, Earley Gate, Reading, RG6 6BB, UK
2Department of Meteorology, University of Reading, Earley Gate, Reading, RG6 6BB, UK
3Met Office Hadley Centre, FitzRoy Road, Exeter, EX1 3PB, UK
Abstract. It has been shown previously that one member of the Met Office Hadley Centre single-parameter perturbed physics ensemble – the so-called "low entrainment parameter" member – has a much higher climate sensitivity than other individual parameter perturbations. Here we show that the concentration of stratospheric water vapour in this member is over three times higher than observations, and, more importantly for climate sensitivity, increases significantly when climate warms. The large surface temperature response of this ensemble member is more consistent with a feedback associated with the stratospheric humidity change, rather than high clouds as has been previously suggested. The direct relationship between the bias in the control state (elevated stratospheric humidity) and the cause of the high climate sensitivity (a further increase in stratospheric humidity) lends further doubt as to the realism of this particular integration. This, together with other evidence, lowers the likelihood that the climate system's physical sensitivity might be significantly higher than the likely upper range quoted in the Intergovernmental Panel on Climate Change's fourth assessment report.