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    Great Historical Events That Were Significantly Affected by the Weather: 6 Inundations and the Mild Winter 1672–73 Help Protect Amsterdam from French Conquest

    Source: Bulletin of the American Meteorological Society:;1983:;volume( 064 ):;issue: 007::page 770
    Author:
    Lindgrén, S.
    ,
    Neumann, J.
    DOI: 10.1175/1520-0477(1983)064<0770:GHETWS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In the 17th century, the small Dutch Republic, the union of seven provinces of the northern part of the Low Countries. was the most important country in the world in matters of finance, commerce, and shipping (as well as in the arts, especially painting). Within the Republic. Amsterdam wielded most of the economic power. Louis XIV, King of France, whose rule was characterized by expansionist tendencies, began a war against the Republic in June 1672 (war actually was declared in April of that year). France and her allies, eastern neighbors of the Republic, sent an invading army of about 150 000, as against a hastily collected and poorly trained defense force of 50 000?60 000 Dutch led by Prince William of Orange, who became William III of Holland in July 1672 and King William III of England in 1689. The spring of 1672 was dry and, as a result, the water level in the rivers was low, a fact that facilitated the crossing of water courses by the hostile forces. Within less than a month, most of the eastern sector of the Republic was captured by the invaders. In order to prevent the penetration of the French into the province of Holland, in which Amsterdam was situated, the Dutch resorted to inundating much of their low-lying lands. creating a kind of moat, roughly 20 km wide, about Amsterdam. The French, who were not equipped for crossing wide water areas, decided to wait until the winter when, so they hoped, the cold would freeze the flooded areas and make it possible for them to reach Amsterdam. However, the winter of 1672?73 turned out to be mild on the whole. On 13 December, a frost set in that does not appear to have been excessive. On 27 December, the French began their advance across the ice, but on the 28th the winds turned from cast to west and the milder air and rains caused the ice to thaw. The French returned to their former positions, but with difficulty, losing many men in the process. January was mild altogether. As a result of the mild winter, Amsterdam was saved from French conquest. Our estimates of air temperatures for the two critical months are: December 1672. 3.3°C; and January 1673, 3.4°C. The observed averages for 1735?1834 at Utrecht-DeBilt, however, were 2.4°C and 0.5°C, respectively. Thus, both of the two months of concern appear to have been relatively warm, especially January.
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      Great Historical Events That Were Significantly Affected by the Weather: 6 Inundations and the Mild Winter 1672–73 Help Protect Amsterdam from French Conquest

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4160682
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    contributor authorLindgrén, S.
    contributor authorNeumann, J.
    date accessioned2017-06-09T14:40:06Z
    date available2017-06-09T14:40:06Z
    date copyright1983/07/01
    date issued1983
    identifier issn0003-0007
    identifier otherams-24052.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4160682
    description abstractIn the 17th century, the small Dutch Republic, the union of seven provinces of the northern part of the Low Countries. was the most important country in the world in matters of finance, commerce, and shipping (as well as in the arts, especially painting). Within the Republic. Amsterdam wielded most of the economic power. Louis XIV, King of France, whose rule was characterized by expansionist tendencies, began a war against the Republic in June 1672 (war actually was declared in April of that year). France and her allies, eastern neighbors of the Republic, sent an invading army of about 150 000, as against a hastily collected and poorly trained defense force of 50 000?60 000 Dutch led by Prince William of Orange, who became William III of Holland in July 1672 and King William III of England in 1689. The spring of 1672 was dry and, as a result, the water level in the rivers was low, a fact that facilitated the crossing of water courses by the hostile forces. Within less than a month, most of the eastern sector of the Republic was captured by the invaders. In order to prevent the penetration of the French into the province of Holland, in which Amsterdam was situated, the Dutch resorted to inundating much of their low-lying lands. creating a kind of moat, roughly 20 km wide, about Amsterdam. The French, who were not equipped for crossing wide water areas, decided to wait until the winter when, so they hoped, the cold would freeze the flooded areas and make it possible for them to reach Amsterdam. However, the winter of 1672?73 turned out to be mild on the whole. On 13 December, a frost set in that does not appear to have been excessive. On 27 December, the French began their advance across the ice, but on the 28th the winds turned from cast to west and the milder air and rains caused the ice to thaw. The French returned to their former positions, but with difficulty, losing many men in the process. January was mild altogether. As a result of the mild winter, Amsterdam was saved from French conquest. Our estimates of air temperatures for the two critical months are: December 1672. 3.3°C; and January 1673, 3.4°C. The observed averages for 1735?1834 at Utrecht-DeBilt, however, were 2.4°C and 0.5°C, respectively. Thus, both of the two months of concern appear to have been relatively warm, especially January.
    publisherAmerican Meteorological Society
    titleGreat Historical Events That Were Significantly Affected by the Weather: 6 Inundations and the Mild Winter 1672–73 Help Protect Amsterdam from French Conquest
    typeJournal Paper
    journal volume64
    journal issue7
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1983)064<0770:GHETWS>2.0.CO;2
    journal fristpage770
    journal lastpage778
    treeBulletin of the American Meteorological Society:;1983:;volume( 064 ):;issue: 007
    contenttypeFulltext
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