THE EFFECT OF ROUGHNESS ELEMENTS ON WIND EROSION THRESHOLD

被引:398
作者
RAUPACH, MR
GILLETTE, DA
LEYS, JF
机构
[1] CSIRO, CTR ENVIRONM MECH, GPO BOX 821, CANBERRA, ACT 2601, AUSTRALIA
[2] NOAA, GEOPHYS LAB CLIMATE CHANGE, AIR RESOURCES LAB, BOULDER, CO 80303 USA
[3] DEPT CONSERVAT & LAND MANAGEMENT, BURONGA, NSW 2648, AUSTRALIA
关键词
D O I
10.1029/92JD01922
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A theory is developed to describe the dependence upon roughness density of the threshold friction velocity ratio R(t), the ratio of the threshold friction velocity of an erodible surface without roughness to that of the surface with nonerodible roughness present. The roughness density is quantified by the frontal area index lambda. The prediction is R(t) = (1 - msigmalambda)-1/2(1 + mbetalambda)-1/2 , where beta is the ratio of the drag coefficient of an isolated roughness element on the surface to the drag coefficient of the substrate surface itself; sigma is the basal-to-frontal area ratio of the roughness elements; and m (< 1) is a parameter accounting for differences between the average substrate surface stress and the maximum stress on the surface at any one point. The prediction is well verified by four independent data sets.
引用
收藏
页码:3023 / 3029
页数:7
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