The impact of anthropogenic climate change is felt most acutely during extreme weather and climate events, such as windstorms, heavy precipitation, flooding, heatwaves, and drought. Applied research in extremes addresses the questions of (a) quantifying the probability of extreme event occurrence and detecting changes over time, (b) attributing such changes to natural variability as well as natural and anthropogenic forcing, including event attribution for individual observed extremes, (c) predicting occurrence probabilities at lead times of days to decades, and (d) deriving centennial and longer climate-change projections (Seneviratne et al., 2021). Designing and interpreting these kinds of studies is underpinned by, and advances, understanding of the physical processes involved.All of these applications are also heavily reliant on computer simulation. For example, large ensembles of global climate model simulations are driven with transient historical and scenario forcings to detect forced changes in the historical period and in projected future climates (Deser et al., 2020), and systematic variation of the natural and anthropogenic forcings used in model experiments allows for the attribution of trends in extremes to these forcings (Wan et al., 2019). Similarly, event attribution contrasts the occurrence of specific historically observed extremes in ensembles of all-forcings simulations and counterfactual simulations in which changing anthropogenic forcings are disregarded (Otto et al., 2018). In forecast applications, ensembles of simulations are initialized with observation-based estimates of the state of the atmosphere, ocean, cryosphere, and land surface with one aim to quantify changes of extreme event occurrence probability in the forecast period compared to a climatological baseline (Davini et al., 2021).Conducting these model experiments is costly in terms of human and computer time, data analysis and storage, and energy consumption. The nature and rareness of the investigated events imposes competing demands on a modeling setup that is fit-for-purpose in terms of model complexity, the length and number of simulations (ensembles members), and resolution. A case in point are seasonal precipitation extremes in the midlatitudes (M. D. K.