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The effect of a well resolved stratosphere on surface climate: Differences between CMIP5 simulations with high and low top versions of the Met Office climate model, , , , and . J. Climate, (May 11, 2012)The Met Office Unified Model Global Atmosphere 4.0 and JULES Global Land 4.0 configurations, , , , , , , , , and 18 other author(s). Geoscientific Model Development, 7 (1): 361--386 (Feb 20, 2014)Multimodel climate and variability of the stratosphere, , , , , , , , , and 32 other author(s). Journal of Geophysical Research, (March 2011)The HadGEM2 family of Met Office Unified Model climate configurations, , , , , , , , , and 41 other author(s). Geoscientific Model Development, 4 (3): 723--757 (Sep 7, 2011)The impact of strong El Niño and La Niña events on the North Atlantic, , , , , , and . Geophysical Research Letters, (February 2019)The Met Office Unified Model Global Atmosphere 4.0 and JULES Global Land 4.0 configurations, , , , , , , , , and 18 other author(s). Geoscientific Model Development Discussions, 6 (2): 2813--2881 (May 14, 2013)The HadGEM2-ES implementation of CMIP5 centennial simulations, , , , , , , , , and 27 other author(s). Geoscientific Model Development, 4 (3): 543--570 (Jul 1, 2011)TI - Robust but weak winter atmospheric circulation response to future Arctic sea ice loss, , , , , , , , , and 22 other author(s). JO - Nature Communications, (2022)