The severe winter in Europe 1941-42: the large-scale circulation, cut-off lows, and blocking

Abstract

The role of quasi-stationary waves during this winter has been studied by decomposing the 500-mb geopotential height data in a low-pass, filtered, quasi-stationary part and a travelling part. The phase of the quasi-stationary wave was such that a ridge was present over the eastern Atlantic and a trough over western Russia throughout most of the winter. As a result the majority of migratory cyclones that approached Europe from the west were steered either south toward the Mediterranean or north of Scandinavia. The synoptic course of events during an outbreak of unusually cold air from the northeast at the end of January 1942 is described in some detail. Some comments are given on how the severe winter weather affected the war in the USSR. -from Author