The reduction of horizontal wind speed at hub height in an infinite cl
uster of wind turbines is computed from a balance between a loss of ho
rizontal momentum due to the drag and replenishment from above by turb
ulent fluxes. This reduction is derived without assumptions concerning
the vertical wind profile above or below hub height, only some basic
assumptions on turbulent exchange have been made. Two applications of
the result are presented, one considering wind turbines and one pressu
re drag on orographic obstacles in the atmospheric boundary layer. Bot
h applications are basically governed by the same kind of momentum bal
ance.