Abstract

For those involved in planning for regional and local scale changes in future climate, there is a requirement for climate information to be available in a context more usually associated with meteorological timescales. Here we combine a tool used in numerical weather prediction, the 30 weather patterns produced by the Met Office, which are already applied operationally to numerical weather prediction models, to assess changes in the UK Climate Projections (UKCP) Global ensemble. Through assessing projected changes in the frequency of the weather patterns at the end of the 21st Century, we determine that future changes in large-scale circulation tend towards an increase in winter of weather patterns associated with cyclonic and westerly wind conditions at the expense of more anticyclonic, settled/blocked weather patterns. In summer, the results indicate a shift towards an increase in dry settled weather types with a corresponding reduction in the wet and windy weather types. Climatologically this suggests a shift towards warmer, wetter winters and warmer, drier summers; which is consistent with the headline findings from the UK Climate Projections 2018. This paper represents the first evaluation of weather patterns analysis within UKCP Global. It provides a detailed assessment of the changes in these weather patterns through the 21st Century and how uncertainty in emissions, structural and perturbed parameters affects these results. We show that the use of these weather patterns in tandem with the UKCP projections is useful for future work investigating changes in a range of weather-related climate features such as extreme precipitation.

Highlights

  • The increasing temporal and spatial resolution of climate models is enabling models to resolve smaller, more intense mesoscale weather features; opening up the opportunity for assessments of how changes in climate will influence the weather

  • An alternative approach could be to utilise the distribution of large-scale circulation features, given these meteorological variables are governed by the large-scale circulation patterns which drive the type of weather a particular region experiences; we can explore whether projected changes in weather patterns could potentially be used to understand future climate hazards

  • To assess changes into the future, the simulated weather patterns for the Analysis Period at the end of the 21st Century are compared to the weather patterns simulated for the Historical Period with a focus on the winter and summer seasons, which display the strongest signal in the distribution of the weather patterns

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Summary

Introduction

The increasing temporal and spatial resolution of climate models is enabling models to resolve smaller, more intense mesoscale weather features; opening up the opportunity for assessments of how changes in climate will influence the weather. An alternative approach could be to utilise the distribution of large-scale circulation features, given these meteorological variables are governed by the large-scale circulation patterns which drive the type of weather a particular region experiences; we can explore whether projected changes in weather patterns could potentially be used to understand future climate hazards Within this analysis, a weather pattern refers to a specific daily circulation pattern over a defined geographical domain (Neal et al 2016).

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