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Comparison of Methods for Estimation of Regional Actual Evapotranspiration in Data Scarce Regions: Blue Nile Region, Eastern Sudan

机译:数据稀缺地区的区域实际蒸散量估算方法的比较:苏丹东部青尼罗河地区

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摘要

Remote sensing techniques enable estimation of regional evapotranspiration (AE) over large areas instead of point calculation and it also saves resources otherwise invested in monitoring instruments. The aim of this paper is to compare actual evapotranspiration (AE) estimated using the remote sensing method, the modified Thornthwaite water balance method (WB), and the complementary relationship method (GG) in the Blue Nile, Eastern Sudan. The satellite based Surface Energy Balance Algorithm for Land (SEBAL) model is used with Moderate Resolution Imaging Spectroradiometer (MODIS) satellite data to estimate daily AE. The WB method is used as benchmark data when comparing the three methods. The results show that: (1) In the dry season (November-April), the SEBAL and GG methods give higher values than the WB method; (2) during the rainy season (May-October), the three methods give comparable results, where there is better agreement between SEBAL and WB than between GG and WB; (3) the spatial distribution pattern of monthly AE estimated by the SEBAL method during the dry season is mainly determined by the land-use type and whether there is irrigation taking place or not. However, in the rainy season, the spatial distribution pattern of monthly AE is mainly determined by the seasonal spatial distribution pattern of rainfall in the region.
机译:遥感技术可以估算大面积区域的蒸散量(AE),而不是计算点数,还可以节省原本投资在监测仪器上的资源。本文的目的是比较使用遥感方法,改进的桑索威特水平衡法(WB)和互补关系法(GG)估算的苏丹东部青尼罗河的实际蒸散量(AE)。基于卫星的土地表面能平衡算法(SEBAL)模型与中等分辨率成像光谱仪(MODIS)卫星数据一起用于估算每日AE。比较这三种方法时,将WB方法用作基准数据。结果表明:(1)在干旱季节(11月至4月),SEBAL和GG方法的值高于WB方法。 (2)在雨季(5月至10月),这三种方法得出的结果可比,SEBAL与WB之间的一致性比GG与WB之间的一致性更好; (3)干旱季节通过SEBAL法估算的月度AE的空间分布格局主要取决于土地利用类型和是否进行灌溉。但是,在雨季,月AE的空间分布格局主要取决于该地区降雨的季节空间分布格局。

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