Abstract
There are four equations which must he satisfied in a description of the flow, in the two-diinensional case, across a change in surface roughness in the neutrally-stable surface boundary layer: the horizontal and vertical momentum equations, the turbulent energy equation, and the continuity equation. Using variations on the Peterson model, the relative magnitudes of the terms in these equations are examined and the wind and shear-stress profiles predicted by each variant model are compared. The following conclusions are made: