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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 10, issue 15
Atmos. Chem. Phys., 10, 7161-7167, 2010
https://doi.org/10.5194/acp-10-7161-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 10, 7161-7167, 2010
https://doi.org/10.5194/acp-10-7161-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.

  04 Aug 2010

04 Aug 2010

Stratospheric water vapour and high climate sensitivity in a version of the HadSM3 climate model

M. M. Joshi1, M. J. Webb2, A. C. Maycock3, and M. Collins4 M. M. Joshi et al.
  • 1National Centre for Atmospheric Science (NCAS) Climate, University of Reading, Earley Gate, Reading RG6 6BB, UK
  • 2Met Office Hadley Centre, FitzRoy Road, Exeter EX1 3PB, UK
  • 3Department of Meteorology, University of Reading, Earley Gate, Reading RG6 6BB, UK
  • 4College of Engineering, Mathematics and Physical Sciences, University of Exeter, North Park Road, Exeter EX4 4QF, 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 stratospheric humidity change, rather than upper tropospheric 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 is significantly higher than the likely upper range quoted in the Intergovernmental Panel on Climate Change's Fourth Assessment Report.

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