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    The Severe Winter in Europe 1941–42: The Large-scale Circulation, Cut-off Lows, and Blocking

    Source: Bulletin of the American Meteorological Society:;1989:;volume( 070 ):;issue: 003::page 271
    Author:
    Lejenäs, Harald
    DOI: 10.1175/1520-0477(1989)070<0271:TSWIET>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The winter of 1941?42 is known as the coldest European winter of the 20th Century. The temperature was much below normal from the beginning of January until the end of March 1942. Blockings and cut-off lows were frequent, particularly during January and February 1942. 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 traveling 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 Mediterranian 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.
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      The Severe Winter in Europe 1941–42: The Large-scale Circulation, Cut-off Lows, and Blocking

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4160918
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    contributor authorLejenäs, Harald
    date accessioned2017-06-09T14:40:38Z
    date available2017-06-09T14:40:38Z
    date copyright1989/03/01
    date issued1989
    identifier issn0003-0007
    identifier otherams-24265.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4160918
    description abstractThe winter of 1941?42 is known as the coldest European winter of the 20th Century. The temperature was much below normal from the beginning of January until the end of March 1942. Blockings and cut-off lows were frequent, particularly during January and February 1942. 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 traveling 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 Mediterranian 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.
    publisherAmerican Meteorological Society
    titleThe Severe Winter in Europe 1941–42: The Large-scale Circulation, Cut-off Lows, and Blocking
    typeJournal Paper
    journal volume70
    journal issue3
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1989)070<0271:TSWIET>2.0.CO;2
    journal fristpage271
    journal lastpage281
    treeBulletin of the American Meteorological Society:;1989:;volume( 070 ):;issue: 003
    contenttypeFulltext
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