When the horizontal resolution is increased in both the atmosphere and the ocean, there are marked improvements in the simulation of the climate of the South East Pacific. This paper will focus on two particular aspects of the simulation in HiGEM. The first of these is the improved representation of coastal upwelling and the stratocumulus decks in the South East Pacific at higher resolution. The second is the more realistic simulation of ENSO, which is largely a result of the improvement in the mean state of the Tropical Pacific due to resolving the heat transport associated with oceanic tropical instability waves.
This paper will also outline the future work with high resolution coupled climate models that is being undertaken as part of VOCALS-UK. The aim of this work is to gain further understanding of how increased resolution can improve the simulation of stratocumulus upwelling regions in global coupled climate models, and the impact that these regions have on the global climate and climate variability.
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