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Probabilistic inference of ecohydrological parameters using observations from point to satellite scales

机译:从点到卫星秤的观测结果的生态学参数的概率推理

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Vegetation controls on soil moisture dynamics are challenging to measure and translate into scale- and site-specific ecohydrological parameters for simple soil water balance models. We hypothesize that empirical probability density functions (pdfs) of relative soil moisture or soil saturation encode sufficient information to determine these ecohydrological parameters. Further, these parameters can be estimated through inverse modeling of the analytical equation for soil saturation pdfs, derived from the commonly used stochastic soil water balance framework. We developed a generalizable Bayesian inference framework to estimate ecohydrological parameters consistent with empirical soil saturation pdfs derived from observations at point, footprint, and satellite scales. We applied the inference method to four sites with different land cover and climate assuming (i) an annual rainfall pattern and (ii) a wet season rainfall pattern with a dry season of negligible rainfall. The Nash-Sutcliffe efficiencies of the analytical model's fit to soil observations ranged from 0.89 to 0.99. The coefficient of variation of posterior parameter distributions ranged from 1 to 15 %. The parameter identifiability was not significantly improved in the more complex seasonal model; however, small differences in parameter values indicate that the annual model may have absorbed dry season dynamics. Parameter estimates were most constrained for scales and locations at which soil water dynamics are more sensitive to the fitted ecohydrological parameters of interest. In these cases, model inversion converged more slowly but ultimately provided better goodness of fit and lower uncertainty. Results were robust using as few as 100 daily observations randomly sampled from the full records, demonstrating the advantage of analyzing soil saturation pdfs instead of time series to estimate ecohydrological parameters from sparse records. Our work combines modeling and empirical approaches in ecohydrol
机译:土壤水分动力学的植被控制是挑战,衡量和转化为简单土壤水平模型的规模和现场特异性生态水论参数。我们假设相对土壤湿度或土壤饱和度的经验概率密度函数(PDF)编码足够的信息以确定这些生态学参数。此外,可以通过对土壤饱和PDF的分析方程的反向建模来估计这些参数,来自常用的随机土壤水平衡框架。我们开发了一种更广泛的贝叶斯推论框架,以估计与在点,足迹和卫星秤的观测结果中达到的经验土壤饱和PDF一致的生态水合学参数。我们将推理方法应用于四个站点,其中包括不同的土地覆盖和气候(i)一年一度的降雨模式和(ii)湿季节降雨模式,降雨量可忽略不计的季节。分析模型的NASH-SUTCLIFFE效率适合土壤观察范围为0.89至0.99。后参数分布的变异系数范围从& 1至15%。在更复杂的季节模型中,参数可识别性并未显着提高;然而,参数值的小差异表明年度模型可能具有吸收的旱季动态。参数估计对于土壤水动力学对感兴趣的拟合生态学参数更敏感的尺度和位置最受约束。在这些情况下,模型反演会聚得更慢,但最终提供了更好的适应性和更低的不确定性。结果使用少数每日观察从完整记录中随机采样,展示了分析土壤饱和PDF而不是时间序列来估计稀疏记录的生态学参数的优点。我们的工作结合了EcoHOWDROL中的建模和经验方法

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