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Fluxes from soil moisture measurements (FluSM v1.0): a data-driven water balance framework for permeable pavements

机译:土壤湿度测量的助熔剂(FLUSM v1.0):用于渗透路面的数据驱动的水平衡框架

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Water fluxes at the soil–atmosphere interface are a key piece of information for studying the terrestrial water cycle. However, measuring and modeling water fluxes in the vadose zone poses great challenges. While direct measurements require costly lysimeters, common soil hydrologic models rely on a correct parametrization, a correct representation of the involved processes, and the selection of correct initial and boundary conditions. In contrast to lysimeter measurements, soil moisture measurements are relatively cheap and easy to perform. Using such measurements, data-driven approaches offer the possibility to derive water fluxes directly. Here we present FluSM (fluxes from soil moisture measurements), which is a simple, parsimonious and robust data-driven water balancing framework. FluSM requires only a single input parameter (the infiltration rate) and is especially valuable for cases where the application of Richards-based models is critical. Since permeable pavements (PPs) present such a case, we apply FluSM on a recently published soil moisture data set to obtain the water balance of 15 different PPs over a period of 2 years. Consistent with findings from previous studies, our results show that vertical drainage dominates the water balance of PPs, while surface runoff plays only a minor role. An additional uncertainty analysis demonstrates the ability of the FluSM-approach for water balance studies, since input and parameter uncertainties only have a small effect on the characteristics of the derived water balances. Due to the lack of data on the hydrologic behavior of PPs under field conditions, our results are of special interest for urban hydrology.
机译:土壤 - 大气接口的水通量是用于研究地面水循环的关键信息。然而,助产区中的测量和建模水助熔剂构成了极大的挑战。虽然直接测量需要昂贵的稳定计,但普通的土壤水文模型依赖于正确的参数化,正确的涉及过程的正确表示,以及选择正确的初始和边界条件。与Lysimeter测量相反,土壤湿度测量相对便宜且易于执行。使用此类测量,数据驱动的方法可以直接提供水通量的可能性。在这里,我们呈现FLUSM(来自土壤湿度测量的助熔剂),这是一种简单,令人统一的数据驱动的水平衡框架。 FLUSM只需要单个输入参数(渗透率),对于理查兹的模型的应用至关重要,尤为有价值。由于透过的路面(PPS)出现这种情况,我们在最近发表的土壤水分数据上涂抹FLUSM,以在2年内获得15种不同PPS的水平衡。我们的结果表明,垂直排水的结果一致,垂直排水占PPS的水平衡,而表面径流仅在次要作用。额外的不确定性分析表明了FLUSM方法用于水平衡研究的能力,因为输入和参数不确定性仅对衍生的水分平衡的特性产生了很小的影响。由于现场条件下缺乏对PPS的水文行为的数据,我们的结果对城市水文有特别感兴趣。

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