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Spatial-temporal evaluation of different reference evapotranspiration methods based on the climate forecast system reanalysis data

机译:基于气候预测系统再分析数据的不同参考蒸发方法的空间 - 时间评估

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Evapotranspiration is a major component of the interaction between land-surface processes and the atmosphere. Climate Forecast System Reanalysis (CFSR) data offer a promising database for overcoming the limitations in availability and reliability of climatological data and, hence, for understanding the evapotranspiration process. Using these data on grid-by-grid daily, seasonal and yearly scales, the present study attempts to advance the spatio-temporal evaluation of two radiation-based and three temperature-based methods for estimating potential evapotranspiration (PET) against estimates of grass reference evapotranspiration (ETo) by FAO Penman-Monteith method (FAO-PM). The analysis was performed for the period 1979-2013, considering the second largest (79 000 km(2)) river system in Ethiopia, that is, Omo-Gibe basin, which accommodates national parks and vast hydropower, cultivation and afforestation developments and discharges its flow to Lake Turkana in Kenya. Despite the large regional variations in climate and elevation, the results in overall emphasize the outperformance of the simple temperature method, viz. Hargreaves-Samani method, in capturing both the annual and seasonal FAO-PM estimates. Calibration of the Hargreaves-Samani equation is, however, a requisite for spectacular improvement of its performance. Accordingly, new coefficients of the equation are proposed. The annual trends in the basin's ETo increased with rising temperature and decreasing relative humidity, wind speed, and solar radiation, but with decreasing (increasing) rainfall in the upper region (the middle and lower regions). It is deduced that trends in simple methods do not necessarily reflect the true trends in ETo. Annual ETo decreases with increasing elevation and annual rainfall. The present findings are discussed in the context of a worldwide literature, thereby improving the understanding of the best performing PET methods in similar data-scarce national or transboundary rivers basin in Ethiopia, the region or worldwide. The wider implications regarding water loss from reservoirs and the rain-fed food and sugar production in the basin under study are also highlighted.
机译:蒸散蒸腾是陆地工艺和大气之间相互作用的主要组成部分。气候预测系统再分析(CFSR)数据提供了一个有前途的数据库,用于克服气候数据的可用性和可靠性的局限性,因此,为了了解蒸发过程。本研究试图利用逐个网格日报,季节性和每年尺度的数据,试图推进两种基于辐射和三种温度的基于辐射和三种温度的方法的时空评估,以估算潜在的蒸散(PET)对草参考的估计粮农组织Penman-Monteith方法(FAO-PM)蒸发(ETO)。考虑到埃塞俄比亚的第二大(79 000公里(2)厘米)河流系统,即Omo-Gibe盆地,该分析是在埃洛·罗宾,即适应国家公园和巨大水电,培养和造林的发展和排放它在肯尼亚到哈蒂卡纳湖流量。尽管气候和海拔的区域变化很大,但总体上的结果强调了简单的温度法,viz的表现。 Hargreaves-Samani方法,在捕获年度和季节性的FAO-PM估计中。然而,Hargreaves-Samani方程的校准是其性能的壮观改善的必要条件。因此,提出了等式的新系数。盆地ETO的年趋势随着温度上升和相对湿度,风速和太阳辐射而增加,但上部区域(中下部和下部)降雨量下降(增加)。推导出简单方法的趋势不一定反映ETO的真正趋势。每年的ETO随着高度提高和年降雨量的增加而减少。在全球文献的背景下讨论了现在的研究结果,从而改善了对埃塞俄比亚,该地区或全世界的类似数据稀缺国家或越境河流盆中的最佳表演宠物方法的理解。还突出了关于水库水库和雨水食品和糖生产的更广泛的影响,还突出了研究。

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