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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Validation of remotely sensed evapotranspiration over the Hai River Basin, China
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Validation of remotely sensed evapotranspiration over the Hai River Basin, China

机译:中国海河流域遥感蒸散量的验证

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摘要

Ground-based validation is crucial for ensuring the accuracy of remotely sensed evapotranspiration (RS-ET) and extending its application. This paper proposes an innovative validation method based on multisource evapotranspiration (ET) from ground measurements, with the validation results including the accuracy assessment, error source analysis, and uncertainty analysis of the validation process. It is a potentially useful approach to evaluate the accuracy and analyze the spatiotemporal properties of RS-ET at both the basin and local scales, and is appropriate to validate RS-ET in diverse resolutions at different time-scales. An independent RS-ET validation using such a method was presented over the Hai River Basin in 2002-2009, China. In general, validation at the basin scale showed good agreements between the 1km annual RS-ET and the validation data such as the water balance ET (root-mean-square error (RMSE): 50.73mm), MODIS ET products (RMSE: 79.84mm), precipitation, and land use types. At the local scale, multiscale ET measurements from large aperture scintillometer (LAS) and eddy covariance system (EC) with a footprint model were used for validation over three typical landscapes. In most cases, the 1km RS-ET resulted in slight overestimation with the LAS measurements (RMSE: 10.75mm for monthly results, 0.78mm for daily results), while the 30m RS-ET was underestimated compared to the EC measurements (RMSE: 16.28mm for monthly results, 0.99mm for daily results). Furthermore, error sources of RS-ET and uncertainties of the validation process were investigated in detail. The results showed that the proposed validation method was reasonable and feasible.
机译:地面验证对于确保遥感蒸散量(RS-ET)的准确性和扩展其应用至关重要。本文提出了一种基于地面测量多源蒸散量(ET)的创新验证方法,验证结果包括验证过程的准确性评估,误差源分析和不确定性分析。在流域和地方尺度上评价RS-ET的准确性和分析其时空特性是一种潜在有用的方法,并且适合在不同的时间尺度上以不同的分辨率验证RS-ET。在2002-2009年的中国海河流域,提出了使用这种方法的独立RS-ET验证。总的来说,流域尺度的验证表明,每年1 km的RS-ET与水平衡ET(均方根误差(RMSE):50.73mm),MODIS ET产品(RMSE:79.84)等验证数据之间具有良好的一致性。毫米),降水量和土地利用类型。在当地范围内,使用大口径闪烁仪(LAS)和涡度协方差系统(EC)以及足迹模型进行的多尺度ET测量用于三个典型景观的验证。在大多数情况下,1公里的RS-ET会导致LAS测量稍有高估(RMSE:月度结果为10.75mm,每日结果为0.78mm),而EC值则将30m RS-ET低估了(RMSE:16.28)毫米(每月结果),0.99毫米(每日结果)。此外,详细研究了RS-ET的错误来源和验证过程的不确定性。结果表明,所提出的验证方法是合理可行的。

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