Climate Change Predictions with a Fully Resolved Stratosphere

Lead Research Organisation: University of Reading
Department Name: Meteorology

Abstract

Climate model simulations for the next assessment of the Intergovernmental Panel on Climate Change (IPCC) are currently being prepared by climate modelling centres around the world. In this joint project with the Met Office, fully coupled atmosphere-ocean model simulations will be performed and analysed using a 'high-top' version of the Met Office Hadley Centre climate model that extends to 85km and therefore fully resolves processes in the stratosphere. Simulations of the past (1860-present) and into the future (to 2100) will be carried out. The project will examine the climate change signals predicted by the fully coupled ocean-troposphere-stratosphere model and investigate the stratospheric influence on surface climate. These aims will be achieved by careful analysis of the model runs, together with additional experiments to isolate processes, test mechanisms and improve statistical significance. Particular emphasis will be placed on (a) regional and seasonal patterns of surface change, especially the North Atlantic Oscillation and impacts over Europe, and (b) detection and attribution studies, exploiting the well-known tropospheric warming / stratospheric cooling signature of anthropogenic influence. Comparisons will be carried out with observations, with corresponding low-top model runs that do not fully resolve the stratosphere and with runs from high-top models carried out by other international climate modelling groups.

Publications

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Charlton-Perez A (2011) On the Use of Geometric Moments to Examine the Continuum of Sudden Stratospheric Warmings in Journal of the Atmospheric Sciences

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Gray L (2016) Eleven-year solar cycle signal in the NAO and Atlantic/European blocking in Quarterly Journal of the Royal Meteorological Society

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Gray L (2012) CORRIGENDUM in Journal of the Atmospheric Sciences

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Gray L (2022) Mechanisms of influence of the Semi-Annual Oscillation on stratospheric sudden warmings in Quarterly Journal of the Royal Meteorological Society

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Hood L (2015) Solar signals in CMIP-5 simulations: the ozone response in Quarterly Journal of the Royal Meteorological Society

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Jones C (2011) The HadGEM2-ES implementation of CMIP5 centennial simulations in Geoscientific Model Development

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Lu H (2011) High- and low-frequency 11-year solar cycle signatures in the Southern Hemispheric winter and spring in Quarterly Journal of the Royal Meteorological Society

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Maycock AC (2015) Possible impacts of a future grand solar minimum on climate: Stratospheric and global circulation changes. in Journal of geophysical research. Atmospheres : JGR

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Mitchell D (2013) Revisiting the controversial issue of tropical tropospheric temperature trends in Geophysical Research Letters

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Mitchell D (2012) The nature of Arctic polar vortices in chemistry-climate models Polar Vortices in Chemistry-Climate Models in Quarterly Journal of the Royal Meteorological Society

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Mitchell D (2014) Signatures of naturally induced variability in the atmosphere using multiple reanalysis datasets in Quarterly Journal of the Royal Meteorological Society