Abstract:We present analytical and numerical calculations of the effective roughness length (ERL) over a flat surface with varying roughness elements, for use in large-scale models. It is shown that ERL is mostly determined by the roughest elements present inside the averaging domain and that, more surprisingly, the ERL increases as the first level of the numerical model gets closer to the surface and its altitude approaches the value of the largest local roughness length. This effect further increases the drag coeffic… Show more
“…These results could be used to specify effective roughness lengths for use in large-scale models. Some of our conclusions differ significantly from those reached recently by Andre and Blondin (1986).…”
Simple calculations of the apparent roughness length for the areally averaged flow over flat but heterogeneous terrain are presented. These results could be used to specify effective roughness lengths for use in large-scale models. Some of our conclusions differ significantly from those reached recently by Andre and Blondin (1986).
“…These results could be used to specify effective roughness lengths for use in large-scale models. Some of our conclusions differ significantly from those reached recently by Andre and Blondin (1986).…”
Simple calculations of the apparent roughness length for the areally averaged flow over flat but heterogeneous terrain are presented. These results could be used to specify effective roughness lengths for use in large-scale models. Some of our conclusions differ significantly from those reached recently by Andre and Blondin (1986).
“…Figures 8, 10, 12 and 14 show that regionally averaged momentum flux is increased by local advection, which is in qualitative agreement with studies by Andre and Blondin (1986), Taylor (1987), Mason (1988) and Claussen (1991). The physical explanation of the momentum flux increase by local advection is that in the case of a variable surface roughness, the rougher zone is exposed to higher wind speeds and the smoother zone to lower wind speeds relative to the adjusted flow.…”
Section: Discussion: Regional Consequences Of Local Advectionsupporting
Abstract. Using a surface-layer model. fluxes of heat and momentum have been calculated for hat regions with regularly spaced step changes in surface roughness and stomata1 resistance. The distance between successive step changes is limited to IO km in order to fill the gap between micro-meteorological measurements and meso-scale models. A single-layer 'big leaf' model of the vegetation is compared with a multi-layer model to assess the performance of the former in the determination of surface fluxes in heterogeneous terrain.The sub-models of vegetation and atmosphere are mainly based on well-known theory. However. a modification of the mixing-length closure of atmospheric exchange is included to achieve a more realistic calculation of fluxes near step changes at the surface. Measurements, presented in the literature. are used to determine the mixing-length parameters and to validate the calculated fluxes downwind of a change in vegetation cover.The single-layer model. well validated for homogeneous surfaces. underestimates the effects of local advection upon the surface fluxes as this model neglects air flow across the edges of tall vegetation. Using the multi-layer model, local advection results in an increase of up to 50% in regional momentum flux and smaller changes in regional evaporation.Even widely spaced heterogeneities appear to influence regional fluxes.
“…In this case, some method of averaging the roughness lengths of different types of surface is required. This problem of calculating an effective roughness length for an area consisting of a patchwork of surfaces with different roughness lengths has recently been discussed by Andre and Blondin (1986), Taylor (1987) and Mason (1988). Taylor (1987) and Mason (1988) have suggested somewhat different ways of forming the average of surface roughness lengths to give an estimate of the effective roughness length of the inhomogeneous surface.…”
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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