The condition hk≪1 says the hill slope is small; ∣∇ϕ∣≪U says the disturbance velocity is small compared with the background wind. Dropping the product ϕxηx and Taylor-shifting the boundary from y=η to y=0 therefore gives
Equivalently, crest minus trough is the negative of this. For kU2/g≪1, hydrostatic elevation dominates; for kU2/g≫1, the Bernoulli pressure drop caused by faster crest flow dominates.