Data presented above is used for computing a boundary
layer profile at the meteo station location (c.f. equation (32)).
As previously referred, information on the height of the boundary
layer is needed only to enforce a constant wind velocity above it.
Once the boundary layer height is specified, the corresponding
wind velocity u∞ is computed from the power-law (29).
Computed data (u∞ and 1 /α ) are displayed, as show at the right