Hostname: page-component-586b7cd67f-rcrh6 Total loading time: 0 Render date: 2024-11-26T03:01:37.726Z Has data issue: false hasContentIssue false

The Diurnal Range of Wind Direction on Ben Nevis

Published online by Cambridge University Press:  06 July 2012

Extract

The weather conditions on the summit of Ben Nevis made it impossible to obtain a continuous record from self-registering anemometers at the Ben Nevis Observatory, but we have in the hourly observations of the wind made by the observers what approximates to a complete and continuous record. The direction and strength of the wind were noted at each hour by day and night, and these observations are to be found tabulated month by month in extenso in this and the preceding volumes of observations. The direction is recorded to 16 points (N., N.N.E., N.E., E.N.E., E., etc.), and the pressure on a scale from 0 to 12 closely akin to the well-known Beaufort scale ; but the situation of the Observatory rendered the record of the wind-pressure or velocity very unsatisfactory.

Type
Appendix
Copyright
Copyright © Royal Society of Edinburgh 1910

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.)

References

page 706 note * See Trans. Roy. Soc. Edin., vol. xliii. p. 483.

page 706 note † See Tables, Trans. Roy. Soc. Edin., vol. xliii. p. 501.

page 706 note ‡ “The Winds of Ben Nevis,” by Omond, R. T. and Rankin, A., Trans. Roy. Soc. Edin., vol. xxxvi. p. 537Google Scholar, and vol. xlii. p. 499.

page 710 note * Compare “St Helena Wind Records,” Annual Report of the Meteorological Committee, London, for the Year ended 31st March 1908, p. 20.

page 710 note † Proc. Roy. Soc. Edin., vol. xiii. p. 839, “The Diurnal Variation in the Direction of the Summer Winds on Ben Nevis,” by R. T. Omond.