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Theoretical Investigation of the Change of Wind Speed along the Axis of a Valley

Theoretische Untersuchung über die Änderung der Windgeschwindigkeit entlang der Achse eines Tales

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Summary

The down valley acceleration of the valley-plain wind is investigated. Under steady state conditions, for short distances along the axis of the valley, there is a linear relationship between the square of the mean velocity of the valley-plain wind and the distance along the axis.

The theory shows that if there is an acceleration along the down-valley direction, the air has to come into the valley at the top in order to preserve continuity of the mass.

Zusammenfassung

Die talabwärts gerichtete Beschleunigung des Bergwindes wird untersucht. Unter stationären Bedingungen gilt für kurze Distanzen entlang der Talachse eine lineare Beziehung zwischen dem Quadrat der mittleren Geschwindigkeit des Bergwindes and dem Abstand entlang der Achse.

Die Theorie zeigt, daß für den Fall einer talabwärts gerichteten Beschleunigung Luft von oben her ins Tal nachgeführt werden muß, um Massenkontinuität zu gewährleisten.

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References

  1. Davidson, B., and P. K. Rao: Preliminary Report on Valley Wind Studies in Vermont, 1957. Final report Contract No. AF 19(604)-1971, Res. Div., College of Engineering, New York University, 1958.

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Additional information

Part of a dissertation in the Department of Meteorology and Oceanography in partial fulfillment of the requirements for the degree of Doctor of Philosophy at New York University.

Part of the research was supported by U. S. Army Signal Research and Development Laboratory, Fort Monmouth, New Jersey, under Contract No. DA-36-039sc-78127.

This paper is dedicated to the late Professor Ben Davidson.

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Rao, P.K. Theoretical Investigation of the Change of Wind Speed along the Axis of a Valley. Arch. Met. Geoph. Biokl. A. 19, 59–70 (1970). https://doi.org/10.1007/BF02274642

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  • DOI: https://doi.org/10.1007/BF02274642

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