Typical logarithmic wind profile in the surface layer, in neutral conditions (Stull 1988). M is the average wind intensity, z the altitude. In the superficial layer the wind speed grows approximately with the logarithm of the height. The profile differs slightly from the logarithmic trend in conditions of unstable stratification.
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Description
1:100 Scale dwg file (meters)
Conversion from meters to feet: a fast and fairly accurate system consists in scaling the drawing by multiplying the value of the unit of measurement in meters by 3.281
 
Details
  • Bioclimatic
  • Format: DWG
  • Size: 2D
  • Download: registered
  • Author: Archweb .com
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