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Some Meteorological Aspects of Flight in the Supersonic Age

Published online by Cambridge University Press:  18 January 2010

C. S. Durst
C. S. Durst
Affiliation:
(Meteorological Consultant)
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Abstract

The main meteorological features of the atmosphere from 50,000 to 70,000 ft. which are likely to be of importance to supersonic aircraft, are the ‘polar-night westerlies’ and the abrupt rises in temperature which take place in late winter in latitudes polewards of 50° or 60°.

The polar-night westerlies blow between 50° and 70° latitude and reach high velocities, increasing with height, from 60,000 ft. during the winter months; towards.the end of the polar night there is often a sudden rise (perhaps as much as 40° C.) at about 85,000 ft., which spreads downwards and is eventually associated with the termination of the polar-night westerlies.

The increase of speed of supersonic aircraft, as well as the decrease of variability of the wind with time at heights above 50,000 ft., have remarkable effects on the punctuality of arrival of aircraft. For instance, on the route from London to New York, the probable error due to wind in arrival time of a 1500-kt. aircraft at 50,000 or 60,000 ft. is about half a minute. This is in contrast with a probable error of ten to fifteen minutes for a 400-kt. aircraft flying at 30,000 ft.

Type
The Prevention of Collision at Sea and in the Air by Shore-And Ground-Based Means
Information
The Journal of Navigation , Volume 15 , Issue 1 , January 1962 , pp. 84 - 90
Copyright
Copyright © The Royal Institute of Navigation 1962

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References

REFERENCES

1Hering, W. S. and Salmela, H. A. (1958). A climatological study of wind and temperature at 100, 50 and 25 mb. &c. Bedford, Mass., G.R.D. Research Notes 1, Article III, p. 19.Google Scholar
2Murgatroyd, R. J. (1957). Winds and temperatures between 20 km. and 100 km. A review, Quart. J.R. met. Soc., 83, 417.CrossRefGoogle Scholar
3Scherhag, R. (1952). Die Explosionartigen Stratosphārenerwarmungen &c., Berichte des Deutschen Wetterdienst in der U.S. Zone, 38, 51–63.Google Scholar
4Craig, R. A. and Hering, W. S. (1958). An explosive warming at 25 mb. in January 1957, Bedford, Mass., G.R.D. Research Notes 1, 81.Google Scholar
5Scrase, F. J. (1953). Relatively high stratospheric temperatures of February 1951, Met. Mag., Lond., 82, 15.Google Scholar
6Muench, H. S. (1958). Temporal variability of stratosphere winds &c. Bedford, Mass., G.D.R. Research Notes 1, 103.Google Scholar
7Durst, C. S. (1954). Variation of wind with time &c. London, M.O. Geoph. Mem., 93.Google Scholar
8Durst, C. S. and Johnson, D. H. (1959). The preparation of statistical wind forecasts &c. London, M.O. Prof. Notes 124.Google Scholar
9Durst, C. S. (1960). The accuracy of upper wind forecasts. This Journal, 13, 288.CrossRefGoogle Scholar
10Durst, C. S. (1959). The probable errors in forecast winds. This Journal, 11, 180.Google Scholar
11Chambers, E. (1959). The jet stream. This Journal, 12, 266.CrossRefGoogle Scholar