Observed wind profiles and turbulence fluxes over an ice surface with changing surface roughness

Wind profile and eddy-correlation data obtained at two sites on a melting g lacier surface in Iceland during the summer of 1996 are presented. Througho ut the experiment the surface roughness increased rapidly from smooth to ve ry rough, with the largest roughness element height obtained being about 1. 7 m. In a layer close to the rough surface we find that the wind speed prof iles were disturbed showing horizontal inhomogeneities as in a roughness su blayer. Its height was approximately two times the height of the main rough ness elements (h) at both sites throughout the experiment. From the wind pr ofiles and eddy-correlation data we calculated corrections for the displace d zero plane as a function of time and compared these with results obtained from a drag partitioning model. In general, the agreement was reasonable c onsidering the ranges of uncertainty but the results indicate that the incr easing horizontal anisotropy of the surface probably limits the use of the model. The values obtained for the roughness lengths are in good agreement with those calculated from a simple linear model, i.e., z(0)/h = 0.5 lambda with lambda the frontal area index. Above the roughness sublayer the wind profiles, normalised standard deviations of wind speed, and the balance of the turbulence kinetic energy budget behaved as over an ideal homogeneous s urface thereby confirming similarity of the flow.