text: The roughness length  appears in the expression for the mean wind speed  near the ground derived using the Monin–Obukhov similarity theory:
  where
  *  is the friction velocity
  *  is the Von Kármán constant
  *  is the elevation (as measured from the ground)
  *  is the elevation of the displacement plane (as measured from the ground), which is an offset that accounts for wind-slowing obstacles such as buildings, trees, or any other structures which impede flow
  *  is the Monin-Obukhov length (which is defined to be the height at which buoyancy and wind shear are equally effective at creating turbulence)
  *  is a correction factor for stability, with  indicating statically neutral conditions. Conditions are statically neutral when the temperature of the air monotonically increases with elevation.
  In the simplest possible case (statically neutral conditions and no wind-slowing obstacles), the mean wind speed simplifies to:
  This provides a method to calculate the roughness length by measuring the friction velocity and the mean wind velocity (at known elevation) in a given, relatively flat location (under neutral conditions) using an anemometer. Of note is that, in this simplified form, the log wind profile is identical in form to the dimensional law of the wall.
  If we don't know the friction velocity, one can calculate the surface roughness as follow
  Due to the limitation of observation instruments and the theory of mean values, the levels (z) should be chosen where there is enough difference between the measurement readings.  If one has more than two readings, the measurements can be fit to the above equation to find the roughness length.
  When calculating the surface roughness, the displacement height can be neglected.