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Reservoir evaporation in a Mediterranean climate: comparing direct methods in Alqueva Reservoir, Portugal

机译:地中海气候中的储层蒸发:比较Alqueva水库的直接方法,葡萄牙

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Alqueva Reservoir is one of the largest artificial lakes in Europe and is a strategic water storage for public supply, irrigation, and energy generation. The reservoir is integrated within the Multipurpose Alqueva Project?(MAP), which includes almost 70?reservoirs in a water-scarce region of Portugal. The MAP contributes to sustainability in southern Portugal and has an important impact on the entire country. Evaporation is the key component of water loss from the reservoirs included in the MAP. Evaporation from Alqueva Reservoir has been estimated by indirect methods or pan evaporation measurements; however, specific experimental parameters such as the pan coefficient were never evaluated. Eddy covariance measurements were performed at Alqueva Reservoir from June to September in?2014 as this time of the year provides the most representative evaporation volume losses in a Mediterranean climate. This period is also the most important period for irrigated agriculture and is, therefore, the most problematic period of the year in terms of managing the reservoir. The direct pan evaporation approach was first tested, and the results were compared to the eddy covariance evaporation measurements. The total eddy covariance (EC)?evaporation measured from June to September?2014 was 450.1?mm. The mean daily EC evaporation in June, July, August, and September was?3.7, 4.0, 4.5, and 2.5?mm?d ?1 , respectively. A pan coefficient, K pan , multivariable function was established on a daily scale using the identified governing factors: air temperature, relative humidity, wind speed, and incoming solar radiation. The correlation between the modelled evaporation and the measured EC?evaporation had an R 2 ?value of?0.7. The estimated K pan ?values were?0.59, 0.57, 0.57, and?0.64 in June, July, August, and September, respectively. Consequently, the daily mean reservoir evaporation?( E Res ) was?3.9, 4.2, 4.5, and 2.7?mm?d ?1 for this 4-month period and the total modelled? E Res was 455.8?mm. The developed K pan ?function was validated for the same period in?2017 and yielded an R 2 ?value of?0.68. This study proposes an applicable method for calculating evaporation based on pan measurements in Alqueva Reservoir, and it can be used to support regional water management. Moreover, the methodology presented here could be applied to other reservoirs, and the developed equation could act as a first evaluation for the management of other Mediterranean reservoirs.
机译:Alqueva水库是欧洲最大的人造湖泊之一,是公共供应,灌溉和能源发电的战略储水。储层集成在多功能Alqueva项目中?(地图),其中包括近70岁的水库在葡萄牙的水资源稀缺区域。该地图有助于葡萄牙南部的可持续性,对整个国家具有重要影响。蒸发是地图中包含的水库的水分损失的关键组成部分。通过间接方法或平移蒸发测量估算了Alqueva水库的蒸发;然而,从未评估了诸如平移系数的特定实验参数。从6月至9月在Alqueva Choploir中进行了涡旋协方差测量?2014年,因为今年的这一时期为地中海气候提供了最具代表性的蒸发量损失。这一时期也是灌溉农业最重要的时期,因此,在管理水库的一年中最有问题的时期。首次测试直接平移蒸发方法,并将结果与​​涡旋协方差蒸发测量进行比较。总涡流协方差(EC)?从6月到9月测量的蒸发2014年为450.1?mm。平均每日EC蒸发在6月,7月,8月和9月是?3.7,4.0,4.5和2.5?m mm?d?1。使用所识别的管理因素,在日常规模中建立平移系数,K盘,多变量功能:空气温度,相对湿度,风速和传入的太阳辐射。模型蒸发与测量的EC之间的相关性蒸发有R 2?值?0.7。估计的K PAN?值为0.59,0.57,0.57,以及6月,7月,8月和9月的0.64分别。因此,每日平均储层蒸发蒸发?(E res)是?3.9,4.2,4.5和2.7?m mm?d?1为此4个月的时间和全面建模? E Res 455.8?mm。开发的K PAN?功能在2017年的同一时期验证,并产生了R 2?值?0.68。本研究提出了一种适用于基于Alqueva水库的PAN测量计算蒸发方法,可用于支持区域水管理。此外,这里呈现的方法可以应用于其他储存器,并且开发的方程可以作为对其他地中海储层管理的第一评估。

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