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首页> 外文期刊>Journal of Hydrology >Uncertainty analysis of the Operational Simplified Surface Energy Balance (SSEBop) model at multiple flux tower sites
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Uncertainty analysis of the Operational Simplified Surface Energy Balance (SSEBop) model at multiple flux tower sites

机译:多个通量塔位置的简化运营表面能平衡(SSEBop)模型的不确定性分析

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Evapotranspiration (ET) is an important component of the water cycle - ET from the land surface returns approximately 60% of the global precipitation back to the atmosphere. ET also plays an important role in energy transport among the biosphere, atmosphere, and hydrosphere. Current regional to global and daily to annual ET estimation relies mainly on surface energy balance (SEB) ET models or statistical and empirical methods driven by remote sensing data and various climatological databases. These models have uncertainties due to inevitable input errors, poorly defined parameters, and inadequate model structures. The eddy covariance measurements on water, energy, and carbon fluxes at the AmeriFlux tower sites provide an opportunity to assess the ET modeling uncertainties. In this study, we focused on uncertainty analysis of the Operational Simplified Surface Energy Balance (SSEBop) model for ET estimation at multiple AmeriFlux tower sites with diverse land cover characteristics and climatic conditions. The 8-day composite 1-km MODerate resolution Imaging Spectroradiometer (MODIS) land surface temperature (LST) was used as input land surface temperature for the SSEBop algorithms. The other input data were taken from the AmeriFlux database. Results of statistical analysis indicated that the SSEBop model performed well in estimating ET with an R2 of 0.86 between estimated ET and eddy covariance measurements at 42 AmeriFlux tower sites during 2001-2007. It was encouraging to see that the best performance was observed for croplands, where R2 was 0.92 with a root mean square error of 13 mm/month. The uncertainties or random errors from input variables and parameters of the SSEBop model led to monthly ET estimates with relative errors less than 20% across multiple flux tower sites distributed across different biomes. This uncertainty of the SSEBop model lies within the error range of other SEB models, suggesting systematic error or bias of the SSEBop model is within the normal range. This finding implies that the simplified parameterization of the SSEBop model did not significantly affect the accuracy of the ET estimate while increasing the ease of model setup for operational applications. The sensitivity analysis indicated that the SSEBop model is most sensitive to input variables, land surface temperature (LST) and reference ET (ET0); and parameters, differential temperature (dT), and maximum ET scalar (K-max), particularly during the non-growing season and in dry areas. In summary, the uncertainty assessment verifies that the SSEBop model is a reliable and robust method for large-area ET estimation. The SSEBop model estimates can be further improved by reducing errors in two input variables (ET and LST) and two key parameters (Kmax and dT). (C) 2016 The Authors. Published by Elsevier B.V.
机译:蒸散量(ET)是水循环的重要组成部分-陆地表面的蒸散量将大约60%的全球降水返回到大气中。 ET在生物圈,大气层和水圈之间的能量传输中也起着重要作用。当前区域到全球以及每天到每年的ET估算主要依靠地表能量平衡(SEB)ET模型或由遥感数据和各种气候数据库驱动的统计和经验方法。由于不可避免的输入错误,参数定义不正确以及模型结构不足,这些模型具有不确定性。在AmeriFlux塔站点上对水,能量和碳通量进行的涡度协方差测量提供了评估ET建模不确定性的机会。在这项研究中,我们专注于在具有不同土地覆盖特征和气候条件的多个AmeriFlux塔站点进行ET估算的操作简化表面能平衡(SSEBop)模型的不确定性分析。将8天复合1公里MODerate分辨率成像光谱仪(MODIS)地表温度(LST)用作SSEBop算法的输入地表温度。其他输入数据来自AmeriFlux数据库。统计分析结果表明,SSEBop模型在估计ET方面表现良好,在2001-2007年期间,在42个AmeriFlux塔地点,估计的ET与涡流协方差测量之间的R2为0.86。令人鼓舞的是,在农田中观察到最佳性能,R2为0.92,均方根误差为13毫米/月。来自SSEBop模型的输入变量和参数的不确定性或随机误差导致每月ET估计,跨不同生物群落分布的多个通量塔站点的相对误差小于20%。 SSEBop模型的不确定性在其他SEB模型的误差范围内,这表明SSEBop模型的系统误差或偏差在正常范围内。这一发现表明,SSEBop模型的简化参数化不会显着影响ET估计的准确性,同时增加了用于运营应用的模型设置的简便性。敏感性分析表明,SSEBop模型对输入变量,地表温度(LST)和参考ET(ET0)最为敏感。和参数,温差(dT)和最大ET标量(K-max),尤其是在非生长季节和干旱地区。总而言之,不确定性评估证明SSEBop模型是用于大面积ET估计的可靠且健壮的方法。通过减少两个输入变量(ET和LST)和两个关键参数(Kmax和dT)的误差,可以进一步改善SSEBop模型估计。 (C)2016作者。由Elsevier B.V.发布

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