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The Catastrophic Flood of the Neva River in 1924

机译:1924年涅瓦河灾难性洪水

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摘要

The necessity of simultaneous analysis of the maximum heights for all three catastrophic floods of the Neva River of September 10(21), 1777, November 7 (19), 1842, and September 23, 1924, interconnected by inter elevation measurements was stated earlier [1,2].rnThe flood of 1924 was preceded by abnormal hydrometeorological situation in the Atlantic and Europe caused by a strong cyclone originated on September 13 near the coast of Cuba. The water in the Neva mouth "began to recede" in the morning on September 23, but by 2 p.m. the height reached 180 cm above zero water level. The water rise "was barely discernable" in the interval 2 p.m.-3 p.m., which "allowed the supposition that the water would recede." However, "the water started to flow rapidly, and by 7 p.m it had reached its maximum of about 365 cm (12 feet)." Stormy weather from the sea (with a windflow of 41 m/s) favored this "additional" Neva water rise. The water "began to recede" after 7 p.m., and the Neva "filled the coasts" by the morning [3, p. 23].
机译:早前指出,必须同时分析内娃河的所有三场灾难性洪水的最大高度,并通过高程测量相互关联[9,10月21日,11777年11月7日(19),1842年9月23日[ 1,2] .rn 1924年的洪水发生在9月13日古巴海岸附近的强旋风引发的大西洋和欧洲异常的水文气象形势之前。 9月23日上午,涅瓦河内河口的水开始“退缩”,但到下午2点。高度达到零水位以上180厘米。在下午2时至下午3时的间隔内,水的上升“几乎无法辨认”,这“假定水会后退”。但是,“水开始迅速流动,到了晚上7点,它达到了约365厘米(12英尺)的最大值。”海上的暴风雨天气(风速为41 m / s)有利于这种“额外的”涅瓦河水位上升。晚上7点后,水开始“退缩”,而涅瓦河则在早晨[3,p。3]填满了海岸。 23]。

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  • 来源
    《Doklady Earth Sciences》 |2009年第6期|985-987|共3页
  • 作者

    V. I. Bogdanov; T. I. Malova;

  • 作者单位

    Pulkovo Observatory, Russian Academy of Sciences, St. Petersburg;

    Pulkovo Observatory, Russian Academy of Sciences, St. Petersburg;

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