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Detecting the Response of Irrigation Water Management to Climate by Remote Sensing Monitoring of Evapotranspiration

机译:遥感监测蒸散监测检测灌溉水管理对气候的响应

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摘要

This study on a large irrigation scheme in Morocco addressed a two-fold question: (a) does the local water management authority adapt water releases to atmospheric water demand ET0-P? and (b) does crop actual evapotranspiration respond to inter- and intra-annual variability in water releases? We have evaluated the inter-annual variability of ET0-P during the period 1992−2017 and compared its anomalies (i.e., deviations from average) with anomalies in annual water release. Overall, it appeared that anomalies in water release were consistent with anomalies in ET0-P. The actual evapotranspiration (ETa) was estimated using a time series of multi-spectral satellite image data by applying the Surface Energy Balance (SEBAL) algorithm in a dry, wet, and reference year. We have determined the quartiles of the distribution of the ET0-P time series to identify these three years. The dry year was 2015−2016, the wet year was 2014−2015, and the reference (median of ET0-P) was 2013−2014. Finally, we compared seasonal and annual anomalies in ET0-P, ETa and release, Wd of irrigation water. In the period 1992−2017, the relative anomalies in ET0-P and Wd were similar only in 2000−2001 and 2015−2016. The analysis of anomalies in water inflow and stocks confirmed the response in increased Wd following wet years with higher inflow and replenishment of the reservoir. The response of crop water use to the irrigation water supply was evaluated by comparing anomalies in the ratio of actual to maximum ET, i.e., ETa/ETc with anomalies in Wd. As regards the Sidi Bennour, Faregh, and Gharbia districts, the relative anomalies in ETa/ETc and Wd were consistent, i.e., they had the same sign and comparable magnitude. Overall, the study shows that water delivery Wd responds to inter-annual variability in the pre-irrigation season water inflows into the reservoirs, rather than in ET0-P. On the other hand, actual crop water use, i.e., ETa/ETc, does respond to inter- and intra-annual variability in Wd. This evidence suggests that there is scope for adaptive water management based on a flexible adaptation of water release to inter- and intra-annual variability in water demand.
机译:在摩洛哥的大型灌区本研究解决两方面的问题:(1)不当地水管理机构适应水排放到大气中的水需求ET0-P?和(b)在不放水作物实际蒸散量来响应之间和内部年际变化?期间1992至2017年我们评价ET0-P的年度间变异性和其相比异常(即,从平均的偏差),在年度水释放异常。总体而言,它似乎在水中释放的异常是在ET0-P异常一致。实际蒸散(ETA)用时间序列多光谱卫星图像数据的通过在干燥施加的能量平衡(SEBAL)算法,湿,并参考年估计。我们已经确定了ET0-P的时间序列,以确定这三年的分布的四分位数。干旱年份为2015- 2016年,湿年是2014- 2015年,与参考(ET0-P的中位数)为2013- 2014年。最后,我们比较了ET0-P,ETA和释放,灌溉水的WD季度和年度异常。在期间1992年至2017年,在ET0-P和Wd相对异常仅在2000 - 2001年和2015 - 2016年是相似的。在水流入和股票异常分析,结果确认以下丰水年具有较高的流入和水库的补给增加WD的响应。农作物水分利用到灌溉供水的响应通过在实际最大ET,即,ETA / ETC与WD异常的比率进行比较的异常进行评价。至于西迪本努尔,Faregh和加尔比亚区,埃塔的/ etc和WD相对异常是一致的,即他们有相同的符号和类似的幅度。总体而言,研究表明,水中分娩WD回应年际变化在预灌溉季节水流入水库,而不是在ET0-P。在另一方面,实际的作物用水量,即,ETA /等,确实在WD之间和内部年际变化响应。这些证据表明,有基于水释放到之间和内部的年度变异用水需求灵活调整适应的水资源管理范围。

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