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
Anstey J
(2013)
The Influence of Stratospheric Vortex Displacements and Splits on Surface Climate
in Journal of Climate
Anstey J
(2013)
Multi-model analysis of Northern Hemisphere winter blocking: Model biases and the role of resolution
in Journal of Geophysical Research: Atmospheres
Ayarzagüena B
(2020)
Uncertainty in the Response of Sudden Stratospheric Warmings and Stratosphere-Troposphere Coupling to Quadrupled CO 2 Concentrations in CMIP6 Models
in Journal of Geophysical Research: Atmospheres
Charlton-Perez A
(2011)
On the Use of Geometric Moments to Examine the Continuum of Sudden Stratospheric Warmings
in Journal of the Atmospheric Sciences
Cnossen I
(2011)
Solar signal propagation: The role of gravity waves and stratospheric sudden warmings
in Journal of Geophysical Research
Ermolli I
(2013)
Recent variability of the solar spectral irradiance and its impact on climate modelling
in Atmospheric Chemistry and Physics
Gray L
(2016)
Eleven-year solar cycle signal in the NAO and Atlantic/European blocking
in Quarterly Journal of the Royal Meteorological Society
Gray L
(2012)
CORRIGENDUM
in Journal of the Atmospheric Sciences
Gray L
(2013)
A lagged response to the 11 year solar cycle in observed winter Atlantic/European weather patterns
in Journal of Geophysical Research: Atmospheres
Gray L
(2013)
Stratospheric Variability in Twentieth-Century CMIP5 Simulations of the Met Office Climate Model: High Top versus Low Top
in Journal of Climate