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首页> 外文期刊>Journal of the Indian Society of Remote Sensing >Evaluation of Simplified Surface Energy Balance Index (S-SEBI) Method for Estimating Actual Evapotranspiration in Kangsabati Reservoir Command Using Landsat 8 Imagery
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Evaluation of Simplified Surface Energy Balance Index (S-SEBI) Method for Estimating Actual Evapotranspiration in Kangsabati Reservoir Command Using Landsat 8 Imagery

机译:用Landsat 8图像估算康斯巴迪储层实际蒸散法的简化表面能平衡指数(S-SEBI)方法

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Evapotranspiration (ET) is an important hydrological variable for better irrigation management, water budgeting, and runoff estimation which should be estimated as precisely as possible both in space and time. However, most of the available crop coefficient-based ET computation methods provide point-scale estimates which need upscaling to apply at the catchment or command area scale. This study evaluates the applicability of the simplified surface energy balance index (S-SEBI) method to compute the spatially distributed daily ET in the Kangsabati reservoir command in eastern India considering the crop coefficient-based coupled Hargreaves-Samani (ETc_HG) method as the benchmark. The study is based on two major crops of paddy and potato in the Rabi season of 2015 at 100 surveyed ground truth locations in the selected command area having different crop growth stages and using the site-specific Landsat 8 images on three cloud-free dates. The S-SEBI method shows improved ET estimates during the crop development stage characterized by higher canopy cover than that during the initial crop development stage with lesser canopy cover that traps less radiation. Results revealed that S-SEBI-based ET estimates correlated well with ETc_HG withrand RMSE value of 0.06 and 1.13 mm/day (initial stage), 0.71 and 0.52 mm/day (development stage) and 0.77 and 0.52 (maturity stage) for paddy. Therand RMSE value for potato is found to be better during the development stage (0.43, 0.69 mm/day) than the initial stage (0.17, 0.64 mm/day) in a similar trend with paddy. Therefore, the crop coefficient-based method could be advantageous at point-scale with adequate data availability conditions, whereas the S-SEBI method could be used in data-scarce areas to estimate the spatially distributed ET values.
机译:Evapotranspiration(et)是一个重要的水文变量,可用于更好的灌溉管理,水预算和径流估计,应该在空间和时间尽可能准确地估计。然而,大多数可用的作物系数基于的ET计算方法提供了需要升级的点尺度估计,以在集水区或命令面积尺度上应用。本研究评估了简化的表面能平衡指数(S-SEBI)方法的适用性,以考虑在印度东部的Kangsabati Reservoir命令中计算空间分布的日常等,考虑到基于作物系数的耦合Hargreaves-Samani(etc_hg)方法作为基准测试。该研究基于2015年的Rabi季节的稻田和马铃薯的两大作物,在100张被调查的地面真理位置,其中包括不同的作物生长阶段,并在三个无云日期使用现场特定的Landsat 8图像。 S-SEBI方法显示了在作物开发阶段的改进的ET估计,其特征在于较高的顶篷覆盖,比初始作物开发阶段具有较小的覆盖辐射的初始作物开发阶段。结果表明,基于S-SEBI的ET估计与RED_HG的RED_HG RMSE值相比好,0.06和1.13mm /天(初始阶段),0.71和0.52mm /天(开发阶段)和0.77和0.52(成熟阶段)。在稻田的开发阶段(0.43,0.69毫米/天)的开发阶段(0.43,0.69毫米/天),发现陶氏菌的RMSE值更好(0.17,0.64毫米/天)。因此,基于作物系数的方法可以在具有足够的数据可用性条件的点刻度下是有利的,而S-SEBI方法可以用于数据稀缺区域以估计空间分布的ET值。

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