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An application of time-lag regression technique for assessment of groundwater fluctuations in a regulated river basin: a case study in Northeastern Thailand

机译:时滞回归技术在调节流域地下水波动评估中的应用:以泰国东北部为例

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摘要

Time series techniques have been applied to a wide variety of academic fields, particularly in the fields of economics, environment, and hydrology. This research work deals with application of the time-lag multiple linear regression technique to predicting the groundwater level and salinity fluctuation in a saline but irrigated area in Northeastern Thailand. Regulating gates are constructed to prevent flooding of the river downstream and to provide the surrounding upstream areas with sufficient irrigation water. The technique is essentially based on the lagged correlation between leading variables, i.e. rainfall and river stages, and their corresponding responses, i.e. groundwater depth and salinity. While the rainfall is simulated with a multiple sinusoidal model, the river stage model comprises two components: a single sinusoidal component and a multiple linear regression component implemented with independent variables, i.e. rainfall, regulating gate outflow, and irrigation supply. The shallow groundwater and groundwater salinity fluctuation in the irrigated area are shown by cross-correlation analysis to be dependent upon the surface water regulation and prior rainfall and thus can be simulated by a multiple linear regression with lagged time dependence. Once properly calibrated and verified, the model can perform better matching to the observed data vis-a-vis the conventional multiple linear regression model. The proposed model can also be deployed for forecasting and management of the future groundwater system, especially in situations in which costlier and more complex numerical modeling techniques are inapplicable.
机译:时间序列技术已应用于广泛的学术领域,特别是在经济学,环境和水文学领域。这项研究工作涉及时滞多元线性回归技术在泰国东北盐碱灌溉区的地下水位和盐度波动预测中的应用。修建了调节闸门,以防止下游河水泛滥,并为周围的上游地区提供充足的灌溉水。该技术基本上是基于领先变量(即降雨和河流水位)及其相应的响应(即地下水深度和盐度)之间的滞后相关性。用多正弦模型模拟降雨时,河段模型包括两个分量:一个正弦分量和一个由独立变量实现的多元线性回归分量,即降雨,调节闸门出水和灌溉供应。互相关分析显示,灌溉区的浅层地下水和盐分波动与地表水调节和先前降雨有关,因此可以通过具有滞后时间依赖性的多元线性回归进行模拟。一旦经过适当的校准和验证,该模型可以相对于传统的多元线性回归模型更好地匹配观察到的数据。提出的模型也可以用于未来地下水系统的预测和管理,尤其是在无法使用更昂贵,更复杂的数值建模技术的情况下。

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