Abstract
Recent extreme weather across the globe highlights the need to understand the potential for more extreme events in the present-day, and how such events may change with global warming. We present a methodology for more efficiently sampling extremes in future climate projections. As a proof-of-concept, we examine the UK’s most recent set of national Climate Projections (UKCP18). UKCP18 includes a 15-member perturbed parameter ensemble (PPE) of coupled global simulations, providing a range of climate projections incorporating uncertainty in both internal variability and forced response. However, this ensemble is too small to adequately sample extremes with very high return periods, which are of interest to policy-makers and adaptation planners. To better understand the statistics of these events, we use distributed computing to run three 1000-member initial-condition ensembles with the atmosphere-only HadAM4 model at 60km resolution on volunteers’ computers, taking boundary conditions from three distinct future extreme winters within the UKCP18 ensemble. We find that the magnitude of each winter extreme is captured within our ensembles, and that two of the three ensembles are conditioned towards producing extremes by the boundary conditions. Our ensembles contain several extremes that would only be expected to be sampled by a UKCP18 PPE of over 500 members, which would be prohibitively expensive with current supercomputing resource. The most extreme winters we simulate exceed those within UKCP18 by 0.85 K and 37% of the present-day average for UK winter means of daily maximum temperature and precipitation respectively. As such, our ensembles contain a rich set of multivariate, spatio-temporally and physically coherent samples of extreme winters with wide-ranging potential applications.
| Original language | English |
|---|---|
| Article number | 100419 |
| Number of pages | 13 |
| Journal | Weather and Climate Extremes |
| Volume | 36 |
| Early online date | 25 Feb 2022 |
| DOIs | |
| Publication status | Published - 1 Jun 2022 |
Bibliographical note
Funding Information:NJL was supported by the Natural Environment Research Council (grant no. NE/L002612/1). PAGW was supported by a Natural Environmental Research Council Independent Research Fellowship (grant no. NE/S014713/1). DMHS was supported by the Met Office Hadley Centre Climate Programme funded by BEIS. We thank Myles R. Allen for his input to the initial discussions of this project, and linking the members of this authorship team up. We thank Kuniko Yamazaki for providing base ancillary files from the original UKCP18 PPE runs. We thank Jason Lowe for his helpful comments and suggestions regarding the text. We thank all of the volunteers who have donated their computing time to climateprediction.net to perform the HadAM4 simulations. The UK Climate Resilience programme is supported by the UK Research & Innovation Strategic Priorities Fund UK Climate Resilience programme. The programme is co-delivered by the Met Office and NERC on behalf of UKRI partners AHRC, EPSRC, ESRC.
Funding Information:
We thank all of the volunteers who have donated their computing time to climateprediction.net to perform the HadAM4 simulations. The UK Climate Resilience programme is supported by the UK Research & Innovation Strategic Priorities Fund UK Climate Resilience programme. The programme is co-delivered by the Met Office and NERC on behalf of UKRI partners AHRC, EPSRC, ESRC.
Funding Information:
NJL was supported by the Natural Environment Research Council (grant no. NE/L002612/1 ). PAGW was supported by a Natural Environmental Research Council Independent Research Fellowship (grant no. NE/S014713/1 ). DMHS was supported by the Met Office Hadley Centre Climate Programme funded by BEIS.
Publisher Copyright:
© 2022 The Authors
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
-
SDG 13 Climate Action
Fingerprint
Dive into the research topics of 'Generating samples of extreme winters to support climate adaptation'. Together they form a unique fingerprint.Cite this
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver