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The maximum wind velocity in ξ1 CMa is ≈700 km s−1.
In the process of estimating the parameters by the maximum wind velocity, there are two interrelated optimization processes.
The numerical experiments show that this method can flexibly generate microburst with any maximum wind velocity, and the error meet the requirement set by the user.
Both types of test section are 1 m in height and 1 m in width, and the maximum wind velocity in the test section can be up to 80m/ss.
However, the actual application of IWG cooling is still limited because a few important parameters are still unclear: maximum wind velocity, minimum operational voltage, degradation of corona-discharging electrodes, and optimum electrode geometries.
The wind velocity generated by bats approaching the insect preparation (T. cantans) was measured by means of hot-wire anemometry and resulted in an average maximum wind velocity of 0.58±0.14 m/s (mean of 70 bat approaches, for example see Fig. 4A).
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Besides, from the meteorological point of view, maximum wind velocities directly relate to storms and thunderstorms.
Once the degree of damage to structures and vegetation has been assessed and matched with the appropriate EF-Scale value, the maximum wind velocities within the range associated with the EF-Scale value are assigned.
In the spring, under the prevailing conditions of low soil moisture contents, daily mean wind velocities over 4.0 m s−1, maximum wind velocities over 12.0 m s−1, and daily maximum air temperatures of over 15°C, almost any landscape can produce æolian dust.
The Gumbel model is often used to fit annual maximum wind speed or wind velocity pressure.
This profile of wind enables the probable maximum operating wind velocity profile for a selected wind turbine design to be predicted.
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