THE LOUISVILLE TORNADO.
THE LOUISVILLE TORNADO.
复制标题
路易斯维尔龙卷风。
DOI：
10.1126/science.ns-16.391.58
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发表时间：
1890
期刊：
影响因子：
56.9
通讯作者：
H. A. Hazen
中科院分区：
文献类型：
--
作者：
H. A. Hazen
那么，我们就不必指望在大约相同的数量内再次发生这样的事故，除非龙卷风地区城镇的规模和频率的增加使这种事故发生的机会更频繁。对于最严重的火灾也可以说是如此。就在这场龙卷风之前，其发展的西部和西北部的大气扰动异常明显;以至于所有发生强烈风暴的地区都提前了将近12小时由华盛顿的信号办公室发出警告，说它们可能会发生。中部时间早上7点，也就是托瑙风暴前12小时，风暴中心位于堪萨斯东部。此时气压低于29.1
Grinr ell, then we need not expect such a one again in about the samne number, excepting as an increase in the size and frequency of towns in the tornado regions gives a more fre-quent opportunity for such accidents. This may also be said as true regarding the most serious fires. Just preceding this tornado the atmospheric disturbance to the west and north-west of its development was unusually marked; so much so, that all the region in which the violent stortns occurred were warned of their probable occurrence nearly twelve hours in advance by the Signal Office at Washington. The centre of the general storm at 7 AM (Central time), or twelve hours before the tornaao, was in eastern Kansas. at which point the air-pressure was below 29.1