A comparison of wind speed shears for frontal and undisturbed synoptic conditions

Springer Science and Business Media LLC - Tập 28 - Trang 329-342 - 1984
Ching-Ming Sheih1
1Environmental Research Division, Argonne National Laboratory, Argonne, (USA)

Tóm tắt

Wind speed shear parameters derived from data collected at a 481-m TV tower are computed for disturbed conditions (cold frontal passage), all undisturbed winds, undisturbed high winds, and undisturbed low winds. The exponential values of the wind speed power law for the case of disturbed conditions are found to be smaller than those for the case of all undisturbed winds, for practically all atmospheric stabilities; the largest exponential value (0.45) appears in the undisturbed low wind case at Richardson numbers near 0.25. The largest mean and standard deviations of the wind shear at the lowest layer (7–26 m) are 0.129 and 0.066 s -1, respectively, which occur for the high wind case at near-neutral stability. The most significant differences between the cases of disturbed and all undisturbed winds are that the former has much larger wind speeds and wind shear standard deviations in atmospherically-stable conditions.

Tài liệu tham khảo

Crawford, K. and Hudson, H. R.: 1970, ‘Behavior of Winds in the lowest 1500 Feet in Central Oklahoma: June 1966–May 1967’, US ESSA Tech. Memo. ERLTM-NSSL 48, 57 pp. Doran, J. c.: 1981, ‘Dependence of Vertical Wind Shear Fluctuations on Averaging Times’, Preprints, Fifth Symposium on Turbulence, Diffusion, and Air Pollution, MS, Atlanta, GA, 44–45. Fichtl, G. H.: 1971, ‘Standard Deviation of Vertical Two-point Longitudinal Velocity Differences in the Atmospheric Boundary Layer’, Boundary-Layer Meteorol. 2, 137–151. Fichtl, G. H.: 1972, ‘Probability Distribution of Vertical Longitudinal Shear Fluctuations’, J. Appl. Meteorol. 11, 918–925. Frost, W., Long, B. H., and Turner, R. E.: 1978, ‘Engineering Handbook on the Atmospheric Environmental Guidelines for Use in Wind Turbine Generator Development’, NASA Tech. Paper 1359, NASA, Washington, D.C. 20546, 356 pp. Fujita, T. T.: 1981, ‘Tornadoes and Downbursts in the Contest of Generalized Planetary Scales’, J. Atmos. Sci. 38, 1511–1534. Fujita, T. T. and Byers, H. R.: 1977, ‘Spearhead Echo and Downburst in the Crash of an Airliner’, Mon. Wea. Rev. 105, 129–146. Goff, C. R. and Zittel, W. D.: 1974, ‘The NSSL/WKY-TV Tower Data Collection Program: April–July 1972’, NOAA Tech. Memo. ERL NSSL-68, 48 pp. Heald, R. C. and Mahrt, L.: 1981, ‘The Dependence of Boundary-Layer Shear on Diurnal Variation of Stability’, J. Appl. Meteorol. 20, 859–867. Kusano, K., Suzuki, Y., and Takei, H.: 1969, ‘Vertical Wind Shear in the Lower Layers at the Tokyo International Airport’, WMO Tech. Note No. 93, 169–183. Ramsdell, J. V.: 1978, ‘Wind Shear Fluctuations Downwind of Large Surface Roughness Elements’, J. Appl. Meteorol. 17, 436–443. Sanders, L. D. and Weber, A. H.: 1970, ‘Evaluation of Roughness Lengths at the NSSL-WKY Meteorological Tower’, ESSA Tech. Memo. ERL NSSL-47, 24 pp. Sisterson, D. L. and Frenzen, P.: 1978, ‘Nocturnal Boundary Layer Wind Maxima and the Problem of Wind Power Assessment’, Environ. Sci. and Tech. 12, 218–221.