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    Great Historical Events That Were Significantly Affected by the Weather: 3, The Cold Winter of 1657–58, The Swedish Army Crosses Denmark's Frozen Sea Areas

    Source: Bulletin of the American Meteorological Society:;1978:;volume( 059 ):;issue: 011::page 1432
    Author:
    Neumann, J.
    DOI: 10.1175/1520-0477(1978)059<1432:GHETWS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In the summer of 1657, Denmark launched hostile actions against Sweden. Charles X, king of Sweden, who at the time was engaged in a war in Poland, marched his army at great speed to Jutland, the westernmost part of Denmark. The conquest of Jutland was completed in November 1657, but in the absence of an adequate naval force, Charles X could not carry his campaign to Zealand, the island on which Copenhagen is situated. Unexpectedly, the severe winter of 1657?58 came to his aid. In February 1658 the Little Belt (separating Jutland from the island of Fünen) as well as the Great Belt (separating Fünen from Zealand) froze over completely and, apparently, to a sufficient depth that the Swedish Army was able to cross over the frozen sea areas from Jutland to Zealand and force the Danes to sue for peace. Ice also played a major role in earlier Scandinavian history. Some excerpts are cited from contemporary literature (and diaries) describing the harshness of the winter of 1657?58 in other European countries. Not only rivers, including major rivers, and lakes froze over but also the coastal waters of Flanders and the Netherlands as well as the Danish sea areas. All estimate of the air temperature of the winter of 1657?58 in the Netherlands is also given.
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      Great Historical Events That Were Significantly Affected by the Weather: 3, The Cold Winter of 1657–58, The Swedish Army Crosses Denmark's Frozen Sea Areas

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    contributor authorNeumann, J.
    date accessioned2017-06-09T14:39:45Z
    date available2017-06-09T14:39:45Z
    date copyright1978/11/01
    date issued1978
    identifier issn0003-0007
    identifier otherams-23893.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4160504
    description abstractIn the summer of 1657, Denmark launched hostile actions against Sweden. Charles X, king of Sweden, who at the time was engaged in a war in Poland, marched his army at great speed to Jutland, the westernmost part of Denmark. The conquest of Jutland was completed in November 1657, but in the absence of an adequate naval force, Charles X could not carry his campaign to Zealand, the island on which Copenhagen is situated. Unexpectedly, the severe winter of 1657?58 came to his aid. In February 1658 the Little Belt (separating Jutland from the island of Fünen) as well as the Great Belt (separating Fünen from Zealand) froze over completely and, apparently, to a sufficient depth that the Swedish Army was able to cross over the frozen sea areas from Jutland to Zealand and force the Danes to sue for peace. Ice also played a major role in earlier Scandinavian history. Some excerpts are cited from contemporary literature (and diaries) describing the harshness of the winter of 1657?58 in other European countries. Not only rivers, including major rivers, and lakes froze over but also the coastal waters of Flanders and the Netherlands as well as the Danish sea areas. All estimate of the air temperature of the winter of 1657?58 in the Netherlands is also given.
    publisherAmerican Meteorological Society
    titleGreat Historical Events That Were Significantly Affected by the Weather: 3, The Cold Winter of 1657–58, The Swedish Army Crosses Denmark's Frozen Sea Areas
    typeJournal Paper
    journal volume59
    journal issue11
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1978)059<1432:GHETWS>2.0.CO;2
    journal fristpage1432
    journal lastpage1437
    treeBulletin of the American Meteorological Society:;1978:;volume( 059 ):;issue: 011
    contenttypeFulltext
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