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首页> 外文期刊>Theoretical and applied climatology >Assessment of surface energy balance algorithm for land and operational simplified surface energy balance algorithm over freshwater and saline water bodies in Urmia Lake Basin
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Assessment of surface energy balance algorithm for land and operational simplified surface energy balance algorithm over freshwater and saline water bodies in Urmia Lake Basin

机译:荨麻湖盆地淡水和盐水砂体陆地和运营简化表面能量平衡算法的评估

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摘要

To manage inland water resources, surveying the performance of remote sensing models for estimating the actual evaporation in arid regions is so important. Hence, this study aimed to assess the performance of two energy balance algorithms including surface energy balance algorithm for land (SEBAL) and operational simplified surface energy balance (SSEBop) in freshwater and saline water bodies. Another purpose of the present study was efficiency improvement in hypersaline lakes. In this regard, a practical salinity correction coefficient was used to overcome shortcomings of the selected models over saline Lake. The analysis of yearly lake water budget was used to assess the selected energy balance algorithms' performance with a novel approach. These algorithms were investigated at Shahid Kazemi Dam Reservoir (as a freshwater body) and Urmia Lake (as a hypersaline water body) in Iran. The results showed that two selected algorithms estimated the evaporation rate at the selected freshwater body with a proper accuracy. The results showed the root mean square error for SEBAL result (RMSESEBAL) as 2.0 mm/day, correlation coefficient for SEBAL result (R-SEBAL) as 0.80 mm/day, and RMSESSEBop and R-SSEBop as 1.7 and 0.80 mm/day, respectively. However, these models overestimated evaporation over the hypersaline water body (RMSESEBAL = 88.4 mm/month, R-SEBAL = 0.90 and RMSESSEBop = 39.9 mm/month, R-SSEBop = 0.94). Salinity correction coefficient improved the results as RMSESEBAL = 19.8 mm/month, R-SEBAL = 0.90 and RMSESSEBop = 13.4 mm/month, and R-SSEBop = 0.94. In general, the algorithm performance was improved using the salinity correction coefficient in the chosen hypersaline water body.
机译:为了管理内陆水资源,测量遥感模型的性能,以估算干旱地区的实际蒸发是如此重要。因此,本研究旨在评估两个能量平衡算法的性能,包括淡水和盐水体中的土地(SEBAL)和运行简化表面能量平衡(SSEBOP)的表面能平衡算法。目前研究的另一个目的是患有浓度湖泊的效率。在这方面,使用实际的盐度校正系数来克服所选模型在盐湖上的缺点。对年湖水预算的分析用于评估采用新方法所选能源平衡算法的性能。在Shahid Kazemi坝储层(作为淡水体)和荨麻疹(作为淡紫色水体)进行了研究这些算法。结果表明,两个选定的算法估计了具有适当精度所选淡水体的蒸发速率。结果表明,SEBAL结果(RMSESEBAL)的根均方误差为2.0mm /天,SEBAL结果(R-SEBAL)的相关系数为0.80毫米/天,以及RMSESSEBOP和R-SSEBOP为1.7和0.80毫米/天,分别。然而,这些模型通过宿舍水体升高蒸发(RMSESEBAL = 88.4毫米/月,R-SEBAL = 0.90和RMSESEBOP = 39.9 mm /月,R-SSEBOP = 0.94)。盐度校正系数改善了RMSESEBAL = 19.8毫米/月的结果,R-SEBAL = 0.90和RMSESEBOP = 13.4毫米/月,R-SSEBOP = 0.94。通常,使用所选择的静脉水体中的盐度校正系数改善了算法性能。

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