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A Stochastic Modelling Technique for Groundwater Level Forecasting in an Arid Environment Using Time Series Methods

机译:时间序列方法在干旱环境下地下水位预测的随机建模技术

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摘要

In arid and semi-arid environments, groundwater plays a significant role in the ecosystem. In the last decades, groundwater levels have decreased due to the increasing demand for water, weak irrigation management and soil damage. For the effective management of groundwater, it is important to model and predict fluctuations in groundwater levels. In this study, several time series models were applied to predict groundwater level forecasting in Kashan plain, Isfahan province, Iran. At first, to reduce the calculation volume, the water table depths in 36 piezometric wells were clustered based on the Vard algorithm. Consequently, we categorized the 36 wells into five clusters. For each cluster, five time series models of auto-regressive (AR), moving-average (MA), auto-regressive moving-average (ARMA), auto-regressive integrated moving-average (ARIMA) and seasonal auto-regressive integrated moving-average (SARIMA) were applied. The results showed that the AR model with a two-times lag (AR(2)), shows the best forecasting of groundwater level for 60 months ahead of the five clusters, with a high accuracy of R~2 (0.89,0.89,0.95, 0.95 and 0.75 in clusters 1 to 5, respectively). According to the results, the average groundwater level fluctuation in 2010 and 2016 was 74.58 and 80.71 m, respectively. With these conditions, the groundwater depletion rate would be 1.02 m per year in 2016. We combined several time series models for a better performance of prediction of groundwater level. We can conclude that combining time series models have an advantage in terms of groundwater level forecasting.
机译:在干旱和半干旱环境中,地下水在生态系统中起着重要作用。在过去的几十年中,由于对水的需求增加,灌溉管理薄弱和土壤破坏,地下水位下降了。为了有效管理地下水,对地下水位波动进行建模和预测很重要。在这项研究中,几个时间序列模型被用于预测伊朗伊斯法罕省喀山平原的地下水位预测。首先,为减少计算量,基于Vard算法对36个测压井的地下水位进行了聚类。因此,我们将36口井归为5类。对于每个集群,五个时间序列模型分别是自回归(AR),移动平均(MA),自回归移动平均(ARMA),自回归综合移动平均值(ARIMA)和季节性自回归综合移动均值(SARIMA)。结果表明,具有两次滞后的AR模型(​​AR(2))显示了五个聚类中60个月以来地下水位的最佳预测,其准确度为R〜2(0.89,0.89,0.95 ,分别在簇1到5中分别为0.95和0.75)。根据结果​​,2010年和2016年的平均地下水位波动分别为74.58和80.71 m。在这些条件下,2016年地下水枯竭率将为每年1.02 m。我们结合了多个时间序列模型,以更好地预测地下水位。我们可以得出结论,结合时间序列模型在地下水位预测方面具有优势。

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