Rapid Temporal Changes of Midtropospheric Winds

Francis J. Merceret Applied Meteorology Unit, NASA/Kennedy Space Center, Florida

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Abstract

The statistical distribution of the magnitude of the vector wind change over 0.25-, 1-, 2-, and 4-h periods based on data from October 1995 through March 1996 over central Florida is presented. The wind changes at altitudes from 6 to 17 km were measured using the Kennedy Space Center 50-MHz Doppler radar wind profiler. Quality controlled profiles were produced every 5 min for 112 gates, each representing 150 m in altitude. Gates 28 through 100 were selected for analysis because of their significance to ascending space launch vehicles. The distribution was found to be lognormal. The parameters of the lognormal distribution depend systematically on the time interval. This dependence is consistent with the behavior of structure functions in the f5/3 spectral regime. There is a small difference between the 1995 data and the 1996 data, which may represent a weak seasonal effect.

Corresponding author address: Dr. Francis J. Merceret, Applied Meteorology Unit—NASA, Mail Code PH-B3, Kennedy Space Center, FL 32899.

Abstract

The statistical distribution of the magnitude of the vector wind change over 0.25-, 1-, 2-, and 4-h periods based on data from October 1995 through March 1996 over central Florida is presented. The wind changes at altitudes from 6 to 17 km were measured using the Kennedy Space Center 50-MHz Doppler radar wind profiler. Quality controlled profiles were produced every 5 min for 112 gates, each representing 150 m in altitude. Gates 28 through 100 were selected for analysis because of their significance to ascending space launch vehicles. The distribution was found to be lognormal. The parameters of the lognormal distribution depend systematically on the time interval. This dependence is consistent with the behavior of structure functions in the f5/3 spectral regime. There is a small difference between the 1995 data and the 1996 data, which may represent a weak seasonal effect.

Corresponding author address: Dr. Francis J. Merceret, Applied Meteorology Unit—NASA, Mail Code PH-B3, Kennedy Space Center, FL 32899.

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