Abstract
Data collected over an inhomogeneous semi-rural area are presented. The data are compared with previous surface-layer data to determine how representative the fixed-point flux measurements are of area averages. Departures from the ‘standard’ surface-layer results are found to be relatively small (~10–20%), which supports the concept of a blending height above which the flow ceases to respond to variations in the underlying surface and becomes horizontally homogeneous.
Effective roughness lengths are derived for different wind directions and the relationship between the effective roughness length and upwind surface is examined in the light of recent ideas on averaging surface roughness lengths. It is found that by averaging drag coefficients, realistic values of the effective roughness length can be calculated which are not very sensitive to the precise choice of the component roughness lengths.
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Grant, A.L.M. Surface drag and turbulence over an inhomogeneous land surface. Boundary-Layer Meteorol 56, 309–337 (1991). https://doi.org/10.1007/BF00119210
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DOI: https://doi.org/10.1007/BF00119210