“…It enables us to determine the main synoptic and surface circulation patterns, as well as at different tropospheric levels, based on extensive sea surface pressure and geopotential at 500 hPa and other levels databases, very often reanalysis, which cannot be processed manually (Huth et al, 2008;Esteban et al, 2006). However, multivariate analysis is not a totally objective process, but rather semi-objective, given that thresholds need to be established and that there is a need to choose from different options at different stages of application, such as establishment of the level of variance explained by the components, the number of synoptic types, the use of T or S modes, rotating or not the components obtained (with the choice in this case of the rotation method), using a hierarchical classification or not, etc.…”