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VII.—The Clear-Day Barometric Curve at Ben Nevis

Published online by Cambridge University Press:  14 February 2012

T. R. Tannahill
Affiliation:
University Observatory, Glasgow

Summary

An examination of the Ben Nevis barometric records shows that, when the non-periodic convex variation is eliminated, the clear-day barometric curve differs but little from the normal curve obtained from all days. The results prove that the clear-day excess found by Buchan and Omond is mainly (though not entirely) due to bias in the selection of data.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1941

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References

References to Literature

Bartels, J., 1927. “Uber die atmosphärischen Gezeiten,” Veröff. Preuss. Met. Inst., Abh. 8, nr. 9.CrossRefGoogle Scholar
Bartels, J., 1935. “Random Fluctuations, Persistence, and Quasi-Persistence in Geophysical and Cosmical Periodicities,” Terrestrial Magnetism, vol. xl, pp. 160.Google Scholar
Buchan, A., and Omond, R. T., 1902. “Diurnal Range of the Barometer in Fine and Cloudy Weather,” Trans. Roy. Soc. Edin., vol. xlii, Appendix, pp. 448463.Google Scholar
Buchan, A., and Omond, R. T., 1890-1910. “The Meteorology of the Ben Nevis Observatories,” Trans. Roy. Soc. Edin., vols. xxxiv, xlii-xliv.Google Scholar
Chapman, S., 1936. “The Lunar Atmospheric Tide at Glasgow,” Proc. Roy. Soc. Edin., vol. Ivi, pp. 15.Google Scholar
Fisher, R. A., 1934. Statistical Methods for Research Workers, Edinburgh and London.Google Scholar
Robb, R. A., and Tannahill, T. R., 1939. “Lunar Atmospheric Pressure Variations at Glasgow,” Proc. Roy. Soc. Edin., vol. lix, pp. 8190.Google Scholar