Submitted to: Agricultural and Forest Meteorology
Publication Type: Peer Reviewed Journal
Publication Acceptance Date: September 1, 1999
Publication Date: February 1, 2000
Citation: EICHINGER, W., COOPER, D., KAO, J., CHEN, L.C., HIPPS, L., PRUEGER, J.H. ESTIMATION OF SPATIALLY DISTRIBUTED LATENT HEAT FLUX OVER COMPLEX TERRAIN FROM A RAMAN LIDAR. AGRICULTURAL AND FOREST METEOROLOGY. 2000. v. 105. p. 145-159.
Interpretive Summary: Estimating the loss of water from agricultural surfaces is critical to understanding the potential impacts of land management and changing climate on crop production. The current methods that are used only measure a single location within a field. We evaluated a technique that would allow a measurement over a large area to determine if a laser system called a lidar could be used to map the source of water loss from a surface of the earth covered with vegetation. This study was conducted as part of a study near Tucson, Arizona to characterize a riparian area for water loss. This method provides a measure of the water loss from nearly a square kilometer with the accuracy of other methods. This method could be used to estimate water loss from large areas to help scientists understand the dynamics of different land surfaces and changes in land surfaces induced by management.
A method is presented in which estimates of evoporation may be made over an area approaching three quarters of a square kilometer, with relatively fine (25m) spatial resolution, using three-dimensional measurements of water vapor concentration from a scanning Raman lidar. The method is based upon Monin-Obukhov similarity theory applied to spatially and temporally averaged data. Data from the lidar is used to sense the location and orientation of the surface and the location of the water vapor measurements with respect to that surface. Maps of the spatial distribution of evaporation have been produced showing the evaporation rates at regular intervals throughout the day. The method was applied to the SALSA experimental site during the 1997 summer field campaign. The estimates of evaporation rates made during the campaign compare favorably with estimates made using sap flux methods with RMS differences of 18W/m2. While the method has certain limitations, the three-dimensional character of the data allows for the detection of anomalous situations so that analysts may alter the analysis technique or reject the estimates from the affected regions. This information can be used in a wide variety of ways to study the spatial variations in evaporation caused by changes in soil type and moisture content, canopy type and topography.