2018
DOI: 10.3390/agronomy8040043
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Assessing Olive Evapotranspiration Partitioning from Soil Water Balance and Radiometric Soil and Canopy Temperatures

Abstract: Evapotranspiration (ET c ) partitioning and obtaining of FAO56 dual crop coefficient (K c ) for olive was carried out with the SIMDualKc software application for root zone and topsoil soil water balance based on the dual crop coefficients. A simplified two source-energy balance model (STSEB), based on daily remotely sensed soil and canopy thermal infrared data and retrieval of surface fluxes, also provided information on partitioning ET c for the olive orchard. Both models were calibrated and validated with gr… Show more

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Cited by 4 publications
(5 citation statements)
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References 44 publications
(55 reference statements)
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“…The initial value for Kc-ini, Kc-mid, and Kc-end in W5 was 1.00, 1.33, and 1.09, and the calibrated value was correspondingly 1.00, 1.30, and 0.89, respectively (Table 3). The initial Ze, TEW, and REW was 0.15 m, 30 mm, and 10 mm, respectively, and the calibrated value was 0.10 m, 21 mm, and 8 mm (Table 3), which is similar to the results of Paço et al [15] and Santos [38]. For the soil of sandy loam in the south in the Mediterranean region, Paço et al [15] showed the value of Ze, TEW, and REW was 0.10 m, 18 mm, and 9 mm, respectively.…”
Section: Simdualkc Model Parameterization and Calibrationsupporting
confidence: 86%
See 1 more Smart Citation
“…The initial value for Kc-ini, Kc-mid, and Kc-end in W5 was 1.00, 1.33, and 1.09, and the calibrated value was correspondingly 1.00, 1.30, and 0.89, respectively (Table 3). The initial Ze, TEW, and REW was 0.15 m, 30 mm, and 10 mm, respectively, and the calibrated value was 0.10 m, 21 mm, and 8 mm (Table 3), which is similar to the results of Paço et al [15] and Santos [38]. For the soil of sandy loam in the south in the Mediterranean region, Paço et al [15] showed the value of Ze, TEW, and REW was 0.10 m, 18 mm, and 9 mm, respectively.…”
Section: Simdualkc Model Parameterization and Calibrationsupporting
confidence: 86%
“…For the soil of sandy loam in the south in the Mediterranean region, Paço et al [15] showed the value of Ze, TEW, and REW was 0.10 m, 18 mm, and 9 mm, respectively. Santos [38] reported that the value of Ze, TEW, and REW in sandy loam was 0.10 m, 22 mm, and 8 mm, respectively.…”
Section: Simdualkc Model Parameterization and Calibrationmentioning
confidence: 98%
“…Although information on crop evapotranspiration can be obtained through using various field measurements techniques [14], those involving direct measurements of ET are generally expensive, labour consuming, require appropriate skills of users and are more appropriate for research, that is, for example, measurements of soil water content [15,16], sap-flow [17][18][19] and eddy covariance [18][19][20], which are applied in this study. Differently, crop ET modelling, using commonly observed meteorological data [4], radiometric canopy temperature [21,22], web based sensors networks [23] and remote sensing information [24][25][26][27][28], including using unmanned aerial vehicles [29] might be useful irrigation management tools, namely for irrigation scheduling purposes and to generate mitigation scenarios to face drought and climate change. Example of models applications to olive orchards include WABOL [30], SIMDualKc [19] and HYDRUS 2D [31].…”
Section: Introductionmentioning
confidence: 99%
“…Details on soil water balance equations, adjustments to plant density and height, as well as crop water stress are given in References [17,20]. To calibrate and validate the model [17,20], and support the derivation of olive ET c act and dual K c , the daily sap flow-based T sf data per treatment and year was used, thus comparing T simulated by SIMDualKc (T sim ) with the observed T sf . 70DI sap flow transpiration data (T sf ) from 2013 was used to calibrate the SIMDualKc model and validation was performed with T sf data collected from 70DI in 2014.…”
Section: Et C and Dual K Cmentioning
confidence: 99%
“…A recommended approach for the estimation of IWU and water stress is the dual K c -ET o methodology adopted by FAO56 [16], where for DI strategies the concept of potential crop evapotranspiration (ET c ) are replaced by the ET c (ET c act ), the result of a K c act coefficient derived from a stress coefficient (K s ) and a soil evaporation coefficient K e , i.e., K c act = K s K cb + K e [17][18][19]. The SIMDualKc model [7,20,21] provides such a computational structure [17,18,22]. The implementation of DI strategies also requires knowing the plant water status, preferably determined by plant-based measurement methods [5,21,23].…”
Section: Introductionmentioning
confidence: 99%