首页> 外文期刊>International journal of applied earth observation and geoinformation >Data assimilation of satellite-based actual evapotranspiration in a distributed hydrological model of a controlled water system
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Data assimilation of satellite-based actual evapotranspiration in a distributed hydrological model of a controlled water system

机译:基于卫星的实际蒸散在控制水系统分布水文模型中的数据同化

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摘要

Advances in earth observation (EC) and spatially distributed hydrological modelling provide an opportunity to improve modelling of controlled water systems. In a controlled water system human interference is high, which may lead to incorrect parameterisation in the model calibration phase. This paper analyses whether assimilation of EO actual evapotranspiration (ETa) data can improve discharge simulation with a spatially distributed hydrological model of a controlled water system. The EO ETa estimates are in the form of eight-day ETa composite maps derived from Terra/MODIS images using the ITA-MyWater algorithm. This algorithm is based on the surface energy balance method and is calibrated for this research for a low-lying reclamation area with a heavily controlled water system: the Rijnland area in the Netherlands. Data assimilation (DA) with the particle filter method is applied to assimilate the ETa maps into a spatially distributed hydrological model. The hydrological model and DA framework are applied using the open source software SIMGRO and PCRaster-Python respectively. The analysis is done for a period between July and October 2013 in which a high discharge peak followed a long dry-spell. The assimilation of EC ETa resulted in local differences in modelled ETa compared to simulation without data assimilation, while the area average ETa remained almost the same. The modelled cumulative discharge graphs, with and without DA, showed distinctive differences with the simulation, with DA better matching the measured cumulative discharge. The bias of simulated cumulative discharge to the observed data reduced from 14% to 4% when using DA of EO ETa. These results showed that assimilating EO ETa may not only be effective in the more common applications of soil moisture and crop-growth modelling, but also for improving discharge modelling of controlled water systems. (C) 2016 Elsevier B.V. All rights reserved.
机译:地球观测(EC)和空间分布水文建模的进步提供了改善受控水系统建模的机会。在受控水系统中,人类干扰很高,这可能导致模型校准阶段中的参数不正确。本文分析了EO实际蒸散(ETA)数据的同化是否可以改善具有受控水系统的空间分布水文模型的放电模拟。 EO ETA估计是使用ITA-Mywater算法从Terra / Modis图像派生的八日ETA复合地图的形式。该算法基于表面能平衡法,为该研究进行了校准,用于具有严重控制的水系统的低洼填海区:荷兰的Rijnland地区。利用颗粒滤波器方法的数据同化(DA)应用于将ETA映射同化到空间分布的水文模型中。使用开源软件SIMGRO和PCRaster-Python应用水文模型和DA框架。分析在2013年7月和10月至10月之间进行了一段时间,其中高放电峰遵循了长期的干法。 EC ETA的同化导致模拟ETA的局部差异与模拟无数据同化,而区域均衡仍然是相同的。模型化的累积放电图,具有和不具有DA,显示出与模拟的独特差异,DA更好地匹配测量的累积放电。当使用EO ETA的DA时,模拟累积放电的偏差从14%降至4%。这些结果表明,同化EO ETA可能不仅在土壤水分和作物生长建模的更常见应用中有效,而且可以改善受控水系统的放电建模。 (c)2016年Elsevier B.v.保留所有权利。

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