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A conceptual and statistical approach for the analysis of climate impact on ground water table fluctuation patterns in cold conditions

机译:一种概念和统计方法,用于分析寒冷条件下气候对地下水位波动模式的影响

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摘要

A robust conceptual and statistical approach is presented for the study of ground water table fluctuations with precipitation and temperature as input variables. A conceptual hydrological model was developed to generate daily rainfall, snowmelt and evapotranspiration values and these values were cross-correlated with observed ground water levels to find representative time lags and significant correlations to describe the ground water system. A statistical model linking rainfall, snowmelt, evapotranspiration and ground water level was then developed and validated for an unconfined esker aquifer in boreal environment in central Finland. The model predicted very well fluctuation of ground water level and timing of the minimum and maximum water levels. A future climate change scenario for the years 2010-2039 was subsequently simulated. The simulation indicates higher ground water levels in milder winter climate. This is due to increase in winter recharge. The model provides a new tool to assess the impacts and address the uncertainties related to climate variation and change in complex ground water systems in cold regions with snow cover.
机译:提出了一种可靠的概念和统计方法,用于研究以降水和温度为输入变量的地下水位波动。建立了概念性的水文模型以产生每日降雨量,融雪和蒸散量,这些值与观测到的地下水位相互关联,以找到代表性的时滞,并与描述地下水系统的显着相关性。然后开发了一个将降雨,融雪,蒸散量和地下水位联系起来的统计模型,并针对芬兰中部北部环境中无限制的艾斯克含水层进行了验证。该模型预测了地下水位的波动非常好,最小和最大水位的时序也很好。随后模拟了2010-2039年的未来气候变化情景。模拟表明,在较温和的冬季气候中,地下水位较高。这是由于冬季补给增加。该模型提供了一种新的工具,可用来评估影响并解决与积雪覆盖的寒冷地区的复杂地下水系统中的气候变化和变化有关的不确定性。

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