Di. Cooper et al., Spatial and temporal properties of water vapor and latent energy flux overa riparian canopy, AGR FOR MET, 105(1-3), 2000, pp. 161-183
A scanning, volume-imaging Raman lidar was used in August 1997 to map the w
ater vapor and latent energy flux fields in southern Arizona in support of
the (Semi-Arid Land Surface Atmosphere) SALSA program. The SALSA experiment
was designed to estimate evapotranspiration over a cottonwood riparian cor
ridor and the adjacent mesquite-grass community. The lidar derived water va
por images showed microscale convective structures with a resolution of 1.5
m, and mapped fluxes with 75 m spatial resolution.
Comparisons of water vapor means over cottonwoods and adjacent grasses show
similar values over both surfaces, but the spatial Variability over the co
ttonwoods was substantially higher than over the grasses. Lidar images supp
ort the idea that the enhanced variability over the cottonwoods is reflecte
d in the presence of spatially coherent microscale structures. Interestingl
y, these microscale structures appear to weaken during midday, suggesting p
ossible evidence for stomatal closure. Spatially resolved latent energy flu
xes were estimated from the lidar using Monin-Obukhov gradient technique. T
he technique was validated from sap-flow flux estimates of transpiration, a
nd statistical analysis indicates very good agreement (within +/-15%) with
coincident lidar flux estimates. Lidar derived latent energy maps showed th
at the riparian zone tended to have the highest fluxes over the site. In ad
dition, the spatial variability of 30 min average fluxes were almost as lar
ge as the mean values. Geostatistical techniques where used to compute the
spatial lag lengths, they were found to be between 100 and 200 m.
Determination of such spatially continuous evapotranspiration from such a c
omplex site presents watershed managers with an additional tool to quantify
the water budgets of riparian plant communities with spatial resolution an
d flux accuracy that is compatible with existing hydrologic management tool
s. (C) 2000 Elsevier Science B.V. All rights reserved.