首页> 外文期刊>Journal of Hydrology >Remote sensing-based soil water balance to estimate Mediterranean holm oak savanna (dehesa) evapotranspiration under water stress conditions
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Remote sensing-based soil water balance to estimate Mediterranean holm oak savanna (dehesa) evapotranspiration under water stress conditions

机译:基于遥感的土壤水分平衡,以评估水分胁迫条件下地中海栎大草原(蒸腾腾)的蒸散量

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This paper aims to present the use of a remote sensing-based soil water balance to estimate holm oak woodland evapotranspiration (ET). The model is based on the assimilation of MODIS reflectance-based vegetation indices in the dual crop coefficient methodology. A daily water balance was performed on the root zone soil to estimate plant water stress. The methodology was evaluated with respect to the actual ET measured by eddy covariance in Mediterranean holm oak savanna (dehesa) for five consecutive years (2004-2008).The model adequately reproduced the absolute values and tendencies measured at daily and weekly periods. Root mean square error (RMSE) was 0.50. mm/day for daily values and 2.70. mm/week for weekly accumulated values. The analysis demonstrated the presence of a long period of water stress during the summer and at the beginning of fall. Measured ET dropped during these periods, and the model replicated this tendency accurately, reaching a stress coefficient value close to 0.2.To be operative, the proposed method required low ground data (reference evapotranspiration and precipitation) and the results indicated a simple, robust method that can be used to map ET and water stress in the dehesa ecosystem.
机译:本文旨在介绍基于遥感的土壤水量平衡估算圣栎林地蒸散量(ET)的方法。该模型基于对偶作物系数方法中基于MODIS反射率的植被指数的同化。在根区土壤上进行每日水分平衡以估计植物的水分胁迫。连续5年(2004-2008年)对地中海holm橡木稀树草原(dehesa)中通过涡度协方差测得的实际ET进行了评估,该模型充分再现了每天和每周测得的绝对值和趋势。均方根误差(RMSE)为0.50。毫米/天的每日值和2.70。每周累积值的毫米/周。分析表明,夏季和秋季开始时长期存在水分胁迫。在这期间测得的ET下降,模型精确地重现了这种趋势,应力系数值接近0.2。要进行操作,建议的方法需要低地面数据(参考蒸散和降水),结果表明该方法简单,可靠可以用来绘制德赫萨生态系统中的ET和水分胁迫图。

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