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- W2155991332 abstract "Over 2800 mean wind profiles (data from two mobile micrometeorological stations near Dallas, Texas) were analyzed to test the Monin-Obukhov similarity hypothesis as expressed by the log-linear wind profile. Wind speed and temperature data for eight levels between 25 cm and 32 m were averaged for 5- and 25-min periods. The Monin-Obukhov parameter α′, which is the coefficient of the linear term in the profile, was found to be a function of stability varying from 0.2 to 3.0 in lapse conditions and from 9 to 3 during inversion conditions. However, practical values of α′ for lapse (0.6) and inversions (5.0) conditions are suggested for forecasting mean diabatic wind profiles. The Obukhov ‘gradient length’ L' was found to be a function of height above the ground; therefore, it does not possess complete dynamic similarity. The broad applicability of the log-linear profile is shown by calculating residual variances for each profile as a function of height, wind speed, and stability. An empirical log-power profile was also tested. The preferred power for the diabatic term was unity (or larger) for inversion conditions and approximately 0.5 for lapse conditions. Since the standard error of estimate of the wind speed based on the log-linear profiles was not significantly greater than that based on log-power for the latter case, the log-linear profile appears to be adequate for all stability regimes." @default.
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- W2155991332 date "1965-05-15" @default.
- W2155991332 modified "2023-09-25" @default.
- W2155991332 title "An investigation of the diabatic wind profile of the atmospheric boundary layer" @default.
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- W2155991332 doi "https://doi.org/10.1029/jz070i010p02277" @default.
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