Difference between revisions of "Logarithmic velocity profile"

logarithmic velocity profile

The variation of the mean wind speed with height in the surface boundary layer derived with the following assumptions: 1) the mean motion is one-dimensional; 2) the Coriolis force can be neglected; 3) the shearing stress and pressure gradient are independent of height; 4) the pressure force can be neglected with respect to the viscous force; and 5) the mixing length l depends only on the fluid and the distance from the boundary, l = kz.

Near aerodynamically smooth surfaces, the result is
that is, the logarithmic velocity profile, where u* is the friction velocity and ν the kinematic viscosity. k ≅ 0.4 and has been called the Kármán constant or von Kármán's constant. The equation fails for a height z sufficiently close to the surface. For aerodynamically rough flow, molecular viscosity becomes negligible. The profile is then
z0 is a constant related to the average height ε of the surface irregularities by z0 = ε/30 and is called the aerodynamic roughness length. Another derivation of the logarithmic profile was obtained by Rossby under the assumption that for fully rough flow the roughness affects the mixing length only in the region where z and z0 are comparable. Then l = k(z + z0) and
For statically nonneutral conditions, a stability correction factor can be included (
see equation in definition of aerodynamic roughness length).

Haugen, D. A. 1973. Workshop on Micrometeorology. Amer. Meteor. Soc., 392 pp.

Sutton, O. G. 1953. Micrometeorology. sect. 3.9.

Copyright 2022 American Meteorological Society (AMS). For permission to reuse any portion of this work, please contact permissions@ametsoc.org. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act (17 U.S. Code § 107) or that satisfies the conditions specified in Section 108 of the U.S.Copyright Act (17 USC § 108) does not require AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, require written permission or a license from AMS. Additional details are provided in the AMS Copyright Policy statement.