Hostname: page-component-745bb68f8f-cphqk Total loading time: 0 Render date: 2025-01-28T03:11:11.582Z Has data issue: false hasContentIssue false
  • English
  • Français

VIII.—Lunar Atmospheric Pressure Variations at Glasgow

Published online by Cambridge University Press:  15 September 2014

R. A. Robb  and
T. R. Tannahill
Get access

Extract

1. In a previous communication (Robb and Tannahill, 1935) the lunar atmospheric pressure inequalities at Glasgow for days whose range of pressure was less than or equal to o·1 in. of mercury were investigated. It was found that a large first harmonic was present and that the second harmonic or semi-diurnal component had a phase angle of 285° in contradiction to the phase angle of 90° as predicted by tidal theory.

Type
Proceedings
Information
Proceedings of the Royal Society of Edinburgh , Volume 59 , 1940 , pp. 81 - 90
Copyright
Copyright © Royal Society of Edinburgh 1940

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

References to Literature

Bartels, J., 1927. “Über die atmosphärischen Gezeiten,” Veröff. Preuss. Met. Inst., Abh. 8, Nr. 9.Google Scholar
Becker, L., 1925. “The Climatology of Glasgow,” M.O. Geophys. Mem.. no. 23.Google Scholar
Chapman, S., 1918. “The Lunar Atmospheric Tide at Greenwich, 1854–1917,” Quart. Journ. Roy. Met. Soc., vol. xliv, pp. 271–279.Google Scholar
Chapman, S., 1936. “The Lunar Atmospheric Tide at Glasgow,” Proc. Roy. Soc. Edin., vol. lvi, pp. 1–5.Google Scholar
Chapman, S., and Austin, M., 1934. “The Lunar Atmospheric Tide at Buenos Ayres, 1891–1910,” Quart. Journ. Roy. Met. Soc., vol. lx, pp. 23–28.Google Scholar
Robb, R. A., and Tannahill, T. R., 1935. “The Lunar Atmospheric Pressure Inequalities at Glasgow,” Proc. Roy. Soc. Edin., vol. lv, pp. 91–96.Google Scholar