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A refined index of model performance: A rejoinder

机译:完善的模型性能指标:重新结合

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摘要

Willmott et al. [Willmott CJ, Robeson SM, Matsuura K. 2012. A refined index of model performance. International Journal of Climatology, forthcoming. DOI:10.1002/joc.2419.] recently suggest a refined index of model performance (d_r) that they purport to be superior to other methods. Their refined index ranges from - 1.0 to 1.0 to resemble a correlation coefficient, but it is merely a linear rescaling of our modified coefficient of efficiency (E_1) over the positive portion of the domain of d_r. We disagree with Willmott et al. (2012) that d_r provides a better interpretation; rather, E_1 is more easily interpreted such that a value of E_1 = 1.0 indicates a perfect model (no errors) while E_1 = 0.0 indicates a model that is no better than the baseline comparison (usually the observed mean). Negative values of E_1 (and, for that matter, d_r < 0.5) indicate a substantially flawed model as they simply describe a 'level of inefficacy' for a model that is worse than the comparison baseline. Moreover, while d_r is piecewise continuous, it is not continuous through the second and higher derivatives. We explain why the coefficient of efficiency (E or E_2) and its modified form (E_1) are superior and preferable to many other statistics, including d_r, because of intuitive interpretability and because these indices have a fundamental meaning at zero. We also expand on the discussion begun by Garrick et al. [Garrick M, Cunnane C, Nash JE. 1978. A criterion of efficiency for rainfall-runoff models. Journal of Hydrology 36: 375-381.] and continued by Legates and McCabe [Legates DR, McCabe GJ. 1999. Evaluating the use of "goodness-of-fit" measures in hydrologic and hydroclimatic model validation. Water Resources Research 35(1): 233-241.] and Schaefli and Gupta [Schaefli B, Gupta HV. 2007. Do Nash values have value? Hydrological Processes 21: 2075-2080. DOI: 10.1002/hyp.6825.]. This important discussion focuses on the appropriate baseline comparison to use, and why the observed mean often may be an inadequate choice for model evaluation and development.
机译:威尔莫特等。 [Willmott CJ,Robeson SM,Matsuura K.,2012年。模型性能的精细指数。国际气候学杂志,即将出版。 [DOI:10.1002 / joc.2419。]最近提出了模型性能的改进指标(d_r),据称它们优于其他方法。它们的精确指数范围介于-1.0到1.0之间,类似于相关系数,但这只是我们在d_r域的正部分上修改后的效率系数(E_1)的线性缩放。我们不同意Willmott等人的观点。 (2012)d_r提供了更好的解释;而是更容易地解释E_1,使得E_1 = 1.0的值表示一个完美的模型(没有错误),而E_1 = 0.0的值表示一个模型不比基线比较(通常是观察到的平均值)好。 E_1的负值(因此d_r <0.5)表示模型存在严重缺陷,因为它们仅描述了模型的“无效水平”,该水平低于比较基准。此外,虽然d_r是分段连续的,但它在二阶和更高阶导数中不是连续的。我们解释了为什么效率系数(E或E_2)及其修改形式(E_1)优于并优于许多其他统计数据,包括d_r,因为它们具有直观的解释性,并且这些指标的基本含义为零。我们还将扩展Garrick等人开始的讨论。 [加里克M,坎纳内C,纳什JE。 1978年。降雨径流模型的效率标准。水文学杂志36:375-381。]和由Legates和McCabe继续[Legates DR,McCabe GJ。 1999年。评估在水文和水文气候模型验证中使用“拟合优度”措施。水资源研究35(1):233-241。]和舍弗利和古普塔[Schaefli B,古普塔高压。 2007年。纳什价值观具有价值吗?水文过程21:2075-2080。 DOI:10.1002 / hyp.6825。]。这个重要的讨论集中在使用适当的基线比较上,以及为什么观察到的均值通常对于模型评估和开发来说可能是一个不适当的选择。

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