2016
DOI: 10.1016/j.agwat.2015.11.018
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Combining a water balance model with evapotranspiration measurements to estimate total available soil water in irrigated and rainfed vineyards

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Cited by 61 publications
(33 citation statements)
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“…Some approaches assimilate into the soil water balance models, either water stress estimates based on canopy temperature [99,100] or ET estimates based on SEB models [73,92,95,101], in order to calibrate the fraction of water depleted derived from the water balance model. In a slightly different approach, some authors propose the integration of actual ET values in order to calibrate the soil water balance model in terms of the root zone storage capacity [94,102,103,104]. The rationale of these approaches is that any empirical approach to the plant water stress, or alternative formulations as those based on the canopy temperature, must be equivalent to the soil water stress, a stress index based on the parametrization of the soil properties [101].…”
Section: Remote Sensing-based Estimates Of Evapotranspirationmentioning
confidence: 99%
“…Some approaches assimilate into the soil water balance models, either water stress estimates based on canopy temperature [99,100] or ET estimates based on SEB models [73,92,95,101], in order to calibrate the fraction of water depleted derived from the water balance model. In a slightly different approach, some authors propose the integration of actual ET values in order to calibrate the soil water balance model in terms of the root zone storage capacity [94,102,103,104]. The rationale of these approaches is that any empirical approach to the plant water stress, or alternative formulations as those based on the canopy temperature, must be equivalent to the soil water stress, a stress index based on the parametrization of the soil properties [101].…”
Section: Remote Sensing-based Estimates Of Evapotranspirationmentioning
confidence: 99%
“…Working in similar canopies like vineyards on a trellis system [30] obtained an RMSE equal to 0.45 and 0.76 mm¨day´1 during two consecutive growing seasons comparing EC measurements and ET c derived from a remote sensing-based water balance, using the relationship between NDVI and the single crop coefficient K c . For a variety of rainfed and irrigation vineyards, reference [68] obtained an RMSE lower than 0.65 mm¨day´1 for each analyzed campaign using a satellite-based crop coefficient and one layer soil water balance. In a row structured vineyard, reference [69] obtained an RMSE of 0.47 mm¨day´1 (17% of the measured values) using the single crop coefficient approach based on the FAO-56 tabulated coefficients.…”
Section: Evaluation Of the One Layer Soil Water Balance Model For Estmentioning
confidence: 99%
“…However, applying these methods to fruit trees is of paramount importance [12,13] because the differences in local practices (planting densities, plant architecture, and the management of the crop understory) have a great effect on the actual value of the crop coefficient [14]. Successful evaluations of the estimated ETc using the Kc-VI relationship have been determined for pecan trees [15], vineyards [12,16], and apples [17]. Some of these authors already postulated the desirable use of these approaches for irrigation assessment in operative scenarios.…”
Section: Introductionmentioning
confidence: 99%
“…This relationship was demonstrated to be similar to the Kcb-NDVI described by Bausch and Neale [30] for corn, and the same relationship has been demonstrated valid for the assessment of crop transpiration in several canopies and various climate conditions. In this sense, Campos et al [16,31] demonstrated the aptitude of this relationship to estimate crop transpiration in row-vines in central Portugal and bush-vines in the West of Spain. Campos et al [32,33] evaluated this relationship in Mediterranean savanna (natural vegetation) in the East of Spain.…”
Section: Estimation Of Crop Transpirationmentioning
confidence: 99%