“…For a given region, there may be a wide range of possible large‐scale meteorological conditions due to variations in the strength and location of synoptic‐scale weather features, defined as atmospheric motion with a typical spatial scale of many hundreds of kilometres, such as extratropical cyclones or high‐pressure systems. () Unsupervised learning, or clustering, techniques may be used to codify these large‐scale atmospheric circulation patterns in terms of a relatively small number of distinct modes() defined based on the fields of mean sea‐level pressure (SLP) and geopotential height, for example, for each time instant of interest. To reduce the number of modes for specific applications, a second clustering stage may be applied, akin to Weia and Mohanb and Ohba et al In the meteorological literature, this process is sometimes referred to as “classification,” but we avoid the use of that term here as in broader usage, this term implies a form of supervised learning.…”