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Evaluation of TSEB turbulent fluxes using different methods for the retrieval of soil and canopy component temperatures from UAV thermal and multispectral imagery

Nieto, Héctor, Kustas, William P., Torres-Rúa, Alfonso, Alfieri, Joseph G., Gao, Feng, Anderson, Martha C., White, W. Alex, Song, Lisheng, Alsina, María del Mar, Prueger, John H., McKee, Mac, Elarab, Manal, McKee, Lynn G.
Irrigation science 2019 v.37 no.3 pp. 389-406
algorithms, canopy, energy balance, energy flow, evaporation, evapotranspiration, grapes, heat transfer, irrigation, models, multispectral imagery, net radiation, orchards, remote sensing, rowcrops, soil temperature, spatial data, thermography, transpiration, unmanned aerial vehicles, vegetation, vegetation index, vineyards, California
The thermal-based Two-Source Energy Balance (TSEB) model partitions the evapotranspiration (ET) and energy fluxes from vegetation and soil components providing the capability for estimating soil evaporation (E) and canopy transpiration (T). However, it is crucial for ET partitioning to retrieve reliable estimates of canopy and soil temperatures and net radiation, as the latter determines the available energy for water and heat exchange from soil and canopy sources. These two factors become especially relevant in row crops with wide spacing and strongly clumped vegetation such as vineyards and orchards. To better understand these effects, very high spatial resolution remote-sensing data from an unmanned aerial vehicle were collected over vineyards in California, as part of the Grape Remote sensing and Atmospheric Profile and Evapotranspiration eXperiment and used in four different TSEB approaches to estimate the component soil and canopy temperatures, and ET partitioning between soil and canopy. Two approaches rely on the use of composite [Formula: see text], and assume initially that the canopy transpires at the Priestley–Taylor potential rate. The other two algorithms are based on the contextual relationship between optical and thermal imagery partition [Formula: see text] into soil and canopy component temperatures, which are then used to drive the TSEB without requiring a priori assumptions regarding initial canopy transpiration rate. The results showed that a simple contextual algorithm based on the inverse relationship of a vegetation index and [Formula: see text] to derive soil and canopy temperatures yielded the closest agreement with flux tower measurements. The utility in very high-resolution remote-sensing data for estimating ET and E and T partitioning at the canopy level is also discussed.