Hostname: page-component-78c5997874-v9fdk Total loading time: 0 Render date: 2024-11-05T16:20:01.408Z Has data issue: false hasContentIssue false

Line-Squalls*

Published online by Cambridge University Press:  28 July 2016

M. A. Giblett*
Affiliation:
Airship Meteorology Division, Meteorological Office, Air Ministry

Extract

The subject of “Line-squalls” is one which has not been entirely neglected in the proceedings of this Society, but it has not hitherto been treated in any degree of detail. Sir Napier Shaw, in a lecture delivered on January 7th, 1914, on the subject of “Wind Gusts and the Structure of Aerial Disturbances,” briefly cited the line-squall as a phenomenon involving a violent commotion in the atmosphere, illustrating his remarks by sketches and meteorological records relating to a well-marked instance on October 14th, 1912, at Aberdeen.

Type
Proceedings
Copyright
Copyright © Royal Aeronautical Society 1927

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Footnotes

*

Read by permission of the Director of the Meteorological Office.

References

1. Bjerknes, J. and Solberg, H., “Meteorological conditions for the Formation of Rain.” Geofysiske Publikasjoner, Oslo, Vol. II., No. 3. This and other publications in the same series for information on the “ Polar Front” and for the basis of Figs. 3, 4, 7 and 8.Google Scholar
2. Lempfert, R. G. K. and Corless, R., “ Line-Squalls and Associated Phenomena.” Quarterly Journal of the Royal Meteorological Society, Vol. XXXVI., 1910, pp. 135170. (Fig. 5.)CrossRefGoogle Scholar
3. Exner, F. M., “Dynamische Meteorologie.” 2nd Edition. Vienna, 1925. (Fig. 6.)CrossRefGoogle Scholar
4. Hunt, H. A., Taylor, Griffith and Quayle, E. T., “Climate and Weather of Australia.” Melbourne, 1913. (Fig. 10.)Google Scholar
5. CaptainToynbee, H., “Gales experienced in the Ocean adjacent to the Cape of Good Hope, between Lat. 30° and 50° S. and Long. 10° and 40° E. Report on.Meteorological Office, London. No. 44, 1882.Google Scholar
6. The Marine Observer, Meteorological Office, London. Vol. I., 1924. (Figs. 13 and 14, Photographs of Line-Squall Clouds.)Google Scholar
7. Samuels, L. T., “ An unusual Kite Record.” Bull. American Meteorological Soc., November, 1926. (Direct measurement of vertical atmospheric current in a thunder cloud.)CrossRefGoogle Scholar
8. “ Large Hailstones.” Meteorological Magazine, Meteorological Office, London, November, 1926, p. 240. (Fig. 26, photograph of large hailstones, originally published in the Factory Mutual Record, July, 1926, issued by the Associated Factory Mutual Fire Insurance Companies, Boston, Mass., and supplied to the Meteorological Office by Mr. George F. Lewis, Deputy Fire Marshal of Ontario.)Google Scholar
9. Wegener, A., “Wind—und Wasserhosen in Europa.” Braunschweig, 1917. (Figs. 16, 17, 18, 22, 23, 24, 25.)Google Scholar
10. Ward, R. De C., “The Tornadoes of the United States as Climatic Phenomena.” Quarterly Journal of the Royal Meteorological Society, Vol. XLIII., 1917, pp. 317329. (Fig. 19.)CrossRefGoogle Scholar
11. Hellmann, G., “Wasserhosen auf dem Atlantischen Ocean.” Sitzungsberichte der Preuss. Akad. der Wissenschaften, XXX., 1925, pp. 539544. (Fig. 20.)Google Scholar
12. Durand-Gréville, E., “Boen und Tornadoes.” Met. Zcits., January, 1897, pp. 821. (Fig: 16, Little Rock Barogram.)Google Scholar