Methods are needed to measure the surface fluxes of sensible (H) and latent
heat (E) at large scales. A promising method is scintillometry. Over pastu
re, a near-infrared scintillometer was most sensitive to temperature fluctu
ations whilst a microwave scintillometer was unduly affected by both humidi
ty fluctuations and correlated temperature-humidity fluctuations. Slower ch
anges in path-averaged humidity caused additional signal variance and an ov
erestimation of H and E. Log-amplitude spectra of the microwave scintillome
ter signal showed inertial-convective subrange behavior. In combination, pa
th-averaged E and H could be determined over 3 km.
Independent corroborative measurements of H and E were made at the path mid
point using the eddy covariance technique. For sensible heat, agreement was
within 4% over a measured range 0-300 W m(-2), with a residual standard de
viation of 45 W m(-2). Latent heat agreed at best to within 12% over the ra
nge 0-450 W m(-2) (residual standard deviation of 94 W m(-2)) and an offset
of 30 W m(-2). (C) 2001 Elsevier Science B.V. All rights reserved.