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Adaptability of the GM(1,1) model for simulation of Jinci Springs discharge

机译:GM(1,1)模型对晋ci泉水排放模拟的适应性

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To tackle of the examination problem of the adaptability of GM (1, 1) model to simulate spring discharge, we set up GM (1, 1) models by using different lengths of observed spring discharge data series of Jinci Springs China. Then we evaluate their adaptability by error analysis. Results showed the average errors of GM (1, 1) models declined from three to five dimensions, kept stable from six to fourteen dimensions, and increased sharply from fifteen to twenty dimensions. So GM (1, 1) models from five to fourteen dimensions are adaptable to simulate spring discharge of Jinci Springs. It means that the evolving processes of groundwater system always have relative stable period and GM (1, 1) model can reflect the processes. We also found that the errors after 1992 become larger than before. Meanwhile an important fact is Jinci Springs became dry in 1994. Those facts reveal that the Jinci groundwater system experienced an unstable period before being dry.
机译:为解决GM(1,1)模型对弹簧流量模拟的适应性检验问题,我们使用不同长度的晋Jin温泉中国观测到的弹簧流量数据序列建立了GM(1,1)模型。然后我们通过误差分析来评估它们的适应性。结果表明,GM(1,1)模型的平均误差从3个维度降低到5个维度,从6个维度稳定到14个维度,从15个维度急剧增加到20个维度。因此,从5到14维的GM(1,1)模型适用于模拟晋ci温泉的泉水排放。这意味着地下水系统的演化过程始终具有相对稳定的时期,而GM(1,1)模型可以反映该过程。我们还发现,1992年之后的误差比以前更大。同时,一个重要的事实是晋ci泉于1994年开始变干。这些事实表明晋ci地下水系统在变干之前经历了一个不稳定时期。

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