Based on the revised Catalogue of European Large-Scale Weather Patterns the annual course and the secular variations of the frequency of blocking highs in Europe are treated. Regions of blocking action and those of frequent cold-air centers mutually exclude one another, both corresponding to the orographically influenced asymmetry of the polar vortex.
Based on the revised Catalogue of European Large‐Scale Weather Patterns (1881–1950) the annual course and the secular variations of the frequency of blocking highs in Europe are treated. Regions of blocking action and those of frequent cold‐air centers mutually exclude one another, both corresponding to the orographically influenced asymmetry of the polar vortex.
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