Maintenance of crop residues on the soil surface is promoted as a mana
gement practice for reducing soil erosion by wind and water. Crop resi
due on the soil surface, however, also influences turbulent exchange p
rocesses that affect surface water and energy balances. At present, th
ere are very limited data on the aerodynamic properties of residue-cov
ered surfaces. The objective of this research was to derive estimates
of the aerodynamic properties (momentum roughness length z(0), zero-pl
ane displacement d, and drag coefficient C-d) of fields with standing
corn (Zea mays L.) stubble. Wind speed and air temperature measurement
s were made at six heights above two no-tillage fields near Ames, IA,
in the spring and fall of 1994 and in the spring of 1995. Both sites h
ad standing corn stubble approximately 0.3 m tall at a density of grea
ter than 60 000 stalks ha(-1) and nearly 95% residue cover. An iterati
ve, least-squares linear regression technique was applied to wind prof
iles obtained under neutral atmospheric conditions to determine z(0),
d, and the friction velocity (u). Mean values of z(0) and d for each
of the three measurement periods varied from 11.8 to 24.3 and 119 to 1
69 mm, respectively. The ratios z(0)/h(s) and d/h(s), where hs is the
mean stubble height, averaged 0.058 and 0.53, respectively, for all pr
ofiles. The magnitude of z(0) and d and their weak dependence on wind
speed are consistent with turbulent dow over a surface with sparse, ri
gid roughness elements. The z(0) and C-d were higher for the fall meas
urement period, suggesting that the loose, fresh residue presented a c
omparatively rough surface that was then smoothed by weathering and co
mpaction beneath snow.