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Estimating Evapotranspiration of an Apple Orchard Using a Remote Sensing-Based Soil Water Balance

机译:基于遥感的土壤水平衡估算苹果园的蒸散量

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The main goal of this research was to estimate the actual evapotranspiration (ET c ) of a drip-irrigated apple orchard located in the semi-arid region of Talca Valley (Chile) using a remote sensing-based soil water balance model. The methodology to estimate ET c is a modified version of the Food and Agriculture Organization of the United Nations (FAO) dual crop coefficient approach, in which the basal crop coefficient (K cb ) was derived from the soil adjusted vegetation index (SAVI) calculated from satellite images and incorporated into a daily soil water balance in the root zone. A linear relationship between the K cb and SAVI was developed for the apple orchard K cb = 1.82·SAVI ? 0.07 ( R 2 = 0.95). The methodology was applied during two growing seasons (2010–2011 and 2012–2013), and ET c was evaluated using latent heat fluxes (LE) from an eddy covariance system. The results indicate that the remote sensing-based soil water balance estimated ET c reasonably well over two growing seasons. The root mean square error (RMSE) between the measured and simulated ET c values during 2010–2011 and 2012–2013 were, respectively, 0.78 and 0.74 mm·day ?1 , which mean a relative error of 25%. The index of agreement (d) values were, respectively, 0.73 and 0.90. In addition, the weekly ET c showed better agreement. The proposed methodology could be considered as a useful tool for scheduling irrigation and driving the estimation of water requirements over large areas for apple orchards.
机译:这项研究的主要目标是使用基于遥感的土壤水平衡模型估算位于塔尔卡山谷(智利)半干旱地区的滴灌苹果园的实际蒸散量(ET c)。估算ET c的方法是联合国粮食及农业组织(FAO)双重作物系数法的修正版本,其中基础作物系数(K cb)从计算得出的土壤调整植被指数(SAVI)中得出从卫星图像中提取出来,并纳入根区的每日土壤水平衡中。苹果园K cb与SAVI之间存在线性关系K cb = 1.82·SAVI? 0.07(R 2 = 0.95)。该方法在两个生长季节(2010-2011年和2012-2013年)中得到了应用,并且使用涡度协方差系统的潜热通量(LE)评估了ET c。结果表明,在两个生长季节中,基于遥感的土壤水平衡合理地估计了ET c。在2010–2011年和2012–2013年期间,测得的和模拟的ET c值之间的均方根误差(RMSE)分别为0.78和0.74 mm·day?1,这意味着相对误差为25%。一致性指数(d)的值分别为0.73和0.90。此外,每周ET c表现出更好的一致性。所提出的方法可以被认为是安排苹果园灌溉计划和推动大面积需水量估算的有用工具。

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