Power-law profile
From Glossary of Meteorology
power-law profile
It is an alternative to the logarithmic velocity profile, and the assumptions are the same, with the exception of the form of the dependence of mixing length l on height z. Here Then where is the mean velocity, u* the friction velocity, ν the kinematic viscosity, and For moderate Reynolds numbers, p = 6/7 (the seventh-root profile) is empirically verified, but for large Reynolds numbers p is between this value and unity. It is to be noted that if is proportional to zm, and if the stress is assumed independent of height, then the eddy viscosity νe is proportional to z1-m. These relations are known as Schmidt's conjugate-power laws.
Sutton, O. G. 1953. Micrometeorology. 78–85.