Answers are grounded in this paper and cite their sources.
The similarity theory of an atmospheric boundary layer over a slightly inclined terrain, discussed in an earlier paper (Sorbjan, 1983) is extended to the case of geostrophic wind varying with height. The forms of resistance laws and universal functions are obtained in the cases when the Ekman height or the actual boundary layer height are used as the boundary layer height scales.
No takes yet. Share an insight, caveat, or question.
Zbigniew Sorbjan (1983) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: