Historical simulations with HadGEM3-GC3.1 for CMIP6

• Published in: Journal of Advances in Modeling Earth Systems
• Main Authors: Andrews, Martin B., Ridley, Jeff K., Wood, Richard A., Andrews, Timothy, Blockley, Edward W., Booth, Ben, Burke, Eleanor, Dittus, Andrea J., Florek, Piotr, Gray, Lesley J., Haddad, Stephen, Hardiman, Steven C., Hermanson, Leon, Hodson, Dan, Hogan, Emma, Jones, Gareth S., Knight, Jeff R., Kuhlbrodt, Till, Misios, Stergios, Mizielinski, Matthew S., Ringer, Mark A., Robson, Jon, Sutton, Rowan T.
• Format: Article in Journal/Newspaper
• Language: English
• Published: American Geophysical Union 2020
• Subjects: Ice; Ice Sheet; North Atlantic; permafrost; Sea ice
• Online Access: https://centaur.reading.ac.uk/91172/; https://centaur.reading.ac.uk/91172/8/2019MS001995.pdf; https://centaur.reading.ac.uk/91172/1/869801_1_merged_1588196445.pdf

We describe and evaluate historical simulations which use the third Hadley Centre Global Environment Model in the Global Coupled configuration 3.1 (HadGEM3-GC3.1) model and which form part of the UK's contribution to the sixth Coupled Model Intercomparison Project, CMIP6. These simulations, run at two resolutions, respond to historically evolving forcings such as greenhouse gases, aerosols, solar irradiance, volcanic aerosols, land use, and ozone concentrations. We assess the response of the simulations to these historical forcings and compare against the observational record. This includes the evolution of global mean surface temperature, ocean heat content, sea ice extent, ice sheet mass balance, permafrost extent, snow cover, North Atlantic sea surface temperature and circulation, and decadal precipitation. We find that the simulated time evolution of global mean surface temperature broadly follows the observed record but with important quantitative differences which we find are most likely attributable to strong effective radiative forcing from anthropogenic aerosols and a weak pattern of sea surface temperature response in the low to middle latitudes to volcanic eruptions. We also find evidence that anthropogenic aerosol forcings play a role in driving the Atlantic Multidecadal Variability and the Atlantic Meridional Overturning Circulation, which are key features of the North Atlantic ocean. Overall, the model historical simulations show many features in common with the observed record over the period 1850–2014 and so provide a basis for future in-depth study of recent climate change.