Atmospheric Circulation
ON March 9 and 10, 1887, the barometer rose to 30 92 inches over Iceland-a very exceptional height for that locality at that time of the year. The United States daily maps of the northern hemisphere show that a storm to the southward of this great anticyclone was carried westward a distance of over...
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Veröffentlicht in: | Nature (London) 1890-06, Vol.42 (1075), p.126-126 |
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Format: | Artikel |
Sprache: | eng |
Online-Zugang: | Volltext |
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Zusammenfassung: | ON March 9 and 10, 1887, the barometer rose to 30 92 inches over Iceland-a very exceptional height for that locality at that time of the year. The United States daily maps of the northern hemisphere show that a storm to the southward of this great anticyclone was carried westward a distance of over six hundred miles within twenty-four hours, in a manner similar to that in which West Indian hurricanes follow the course of the trade winds in August and September, although this storm was located in latitude 40° N., or in the usual situation of the anti-trades. Other instances of a similar character have been noted, but this one was unusually well defined, and throws much light upon the laws governing the atmospheric circulation. |
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ISSN: | 0028-0836 1476-4687 |
DOI: | 10.1038/042126c0 |