- 1CSIROEnvironment, Hobart, Australia (chris.chapman@.csiro.au)
- 2Department of Meteorology and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
- 3School of Computing and Mathematical Sciences, University of Leicester, Leicester, UK
We study the hemispheric to continental scale regimes that lead to summertime heatwaves in the Northern Hemisphere. By using a powerful data mining methodology -archetype analysis - we identify characteristic spatial patterns consisting of a blocking high pressure systems embedded within a meandering upper atmosphere circulation that is longitudinally modulated by coherent Rossby Wave Packets. Periods when these atmospheric regimes are strongly expressed correspond to large increases in the likelihood of extreme surface temperature. Most strikingly, these regimes are shown to be typical of surface extremes and frequently reoccur. Three well publicised heatwaves are studied in detail - the June-July 2003 western European heatwave, the August 2010 "Russian" heatwave, and the June 2021 "Heatdome" event across western North America. We discuss the implications of our work for long-range prediction or early warning, climate model assessment and post-event diagnosis.
How to cite: Chapman, C., Monselesan, D., Risbey, J., Hannachi, A., Lucarini, V., and Matear, R.: The Typicality of Regimes Associated with Northern Hemisphere Heatwaves, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-3877, https://doi.org/10.5194/egusphere-egu25-3877, 2025.