Surface Aerodynamic Temperature Derived from Wind/Temperature Profile Measurements over Cotton and Alfalfa in a Semi-Arid Environment

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Assessing the project efficiency of irrigation systems and water use efficiency of crops over large irrigated areas requires daily or seasonal evapotranspiration (ET) maps. Mapping ET or latent heat flux (LE) can be achieved spatially for land surfaces using remote sensing inputs such as surface reflectance and radiometric surface temperature ( T s ). The energy balance (EB) equation requires net radiation ( R n ), soil heat flux ( G ), and sensible heat flux ( H ) to derive LE as a residual. Although R n and G can be estimated with acceptable accuracy, H may be under estimated when T s is used rather than the surface aerodynamic temperature ( T o ) in the aerodynamic resistance equation. The value of T o cannot be measured directly because it varies with atmospheric forcing resulting from radiation, wind speed and air temperature, and with variable surface conditions. In this study, T o for dryland cotton in the Texas High Plains and irrigated alfalfa in Colorado was determined using T s , air temperature, leaf area index, and surface aerodynamic resistance, and ET measurements obtained with large weighing lysimeters. The specific performance of the modeled T o for cotton and alfalfa was assessed using an aerodynamic profile method. Results indicated that the T o model based on aerodynamic resistance better agreed (0.2±1°C) with measured T o values using the aerodynamic profile method.