Aerodynamic resistance to heat transfer (r(ah)) needed to calculate se
nsible heat flux (H) used in energy balance modeling can be estimated
from momentum aerodynamic resistance with corrections for atmospheric
stability. This study compared r(ah) and H modeled by four commonly us
ed resistance methods with r(ah) and H measured indirectly through ene
rgy balance techniques. Three momentum aerodynamic parameters were cal
culated: roughness length, Z(om); zero plane displacement, d; and fric
tion velocity, U. Corn (Zen mays L.) was grown on east-west rows (0.7
5m wide) in 1989 and 1990 at Bushland, TX, in two contiguous 5-ha fiel
ds where two weighing lysimeters were located and micrometeorological
measurements were made. Sensible heat flux was indirectly measured as
a residual of the energy balance and then used to calulate aerodynamic
resistance. Momentum aerodynamic parameters were calculated from near
-neutral condition wind-speed profiles using a least squares procedure
. The momentum parameter relationships to crop height (CH) were d = 0.
73 x CH(r(2) = 0.59) and Z(om) = 0.12 x CH (r(2) = 0.96). While no r(a
h) model performed well, the best linear fit (r(2) = 0.75, y = 1.O8x 4.2) between measured (x) and modeled (y) r(ah) occurred under stable
atmospheric conditions; for measured and modeled H, the best linear f
it (r(2) = 0.84, y = 0.93x + 62.1) occurred under all atmospheric cond
itions. Measured r(ah) in neutral and unstable conditions was not clos
ely associated with wind speed. Performance of a model with a limited
stability factor nas improved by increasing the magnitude of the facto
r, These results suggest that r(ah) models may be sensitive to atmosph
eric stability and local conditions such as fetch and leaf area.