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After checking mean wind profiles below the height of building in tornado flow fields, a kind of spiral was found.
Since the mean wind profile in the tropical cyclone boundary layer is important in both the fields of meteorology and wind engineering, the wind measurements taken during the passages of several tropical cyclones or typhoons in Hong Kong by the wind-profilers and the Doppler Sonic Detection And Ranging (SODAR) have been utilized to calculate both the hourly and 10-min mean wind profiles.
Figure 3 gives the mean wind profiles calculated from rawinsondes data during the field campaign at 08 00, 12 00, 15:00, and 18 00 hs.
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The model reproduces the mean wind profile for any geographic location on any day and at any time of the year.
The results showed that the low-level jet, which is commonly observed for the mean wind profile in the tropical cyclone boundary layer over the sea, was not found.
For one thing, the approaching wind flow adopted in a wind-tunnel topographic study is adjusted according to the mean wind profile extracted from a meso-scale meteorological simulation of Typhoon Fengshen (2008) for a particular period, during which the observed wind direction indicated the sea-fetch wind flow.
The southern states have their average wind profile at 10 m height in the range between 3.0 and 3.5 m/s, contingent upon the states, and northern states fit with mean wind paces of between 4.0 and 7.5 m/s.
Specifically, mean wind velocity profiles and wind direction profiles measured during 16 strong windy days (synoptic wind) are analyzed in the present paper.
The extreme profiles of the turbulence intensities vary as much as 100% along the span, and the mean wind velocity profiles vary up to 50% along the span.
The simulated mean wind velocity profiles and turbulence intensity distributions are plotted in Fig. 1a, b, respectively.
In this paper, the characteristics of the mean wind speed profiles evaluated for each distinguished wind speed in each wind direction were presented.
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