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A qualitative description of shallow groundwater effect on surface temperature of bare soil

机译:定性描述浅层地下水对裸土表面温度的影响

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Whether or not shallow groundwater affects skin temperature (the temperature of soil surface) is important to detect depth and extent of shallow groundwater by dint of remote sensing and important for land surface modelling studies. Although few studies have been conducted to investigate that effect, they have yielded contradicting conclusions and they stopped in 1982. To determine that shallow groundwater affects skin temperature, we measured soil temperature at two different depths (5 and 10 cm) in seven places with variable water table depths every ten minutes and for six days. After that, we correlated the minimum, maximum and average daily temperatures to average groundwater depth. We also built a simple numerical model using a differential equations solver, Flex PDE, to simulate heat transfer into soil profile and used it to simulate groundwater effect on skin temperature. We found quite high negative correlation between the maximum and average daily soil temperature and groundwater depth. Contrarily, we could hardly find any correlation between the daily minimum temperature and groundwater depth. Numerical simulations, though simple, were useful in showing that groundwater shifted skin temperature curves up in the winter and down in the summer without affecting the shape of the curve. We conclude that shallow groundwater affects skin temperature directly by its distinctive thermal properties in the soil profile and indirectly by affecting soil moisture which in turn has many different and contradictory effects on skin temperature. This study recommends building a comprehensive numerical model that simulates the effect of shallow groundwater on skin temperature and on the different energy fluxes at land surface.
机译:浅层地下水是否影响皮肤温度(土壤表面温度)对于通过遥感检测浅层地下水的深度和程度很重要,并且对于土地表面建模研究也很重要。尽管很少进行研究来研究这种影响,但得出的结论却相矛盾,并于1982年终止。为确定浅层地下水对皮肤温度的影响,我们在七个不同深度的两个不同深度(5和10厘米)处测量了土壤温度地下水位每十分钟一次,持续六天。之后,我们将最低,最高和平均每日温度与平均地下水深度相关联。我们还使用微分方程求解器Flex PDE建立了一个简单的数值模型,以模拟热传递到土壤剖面中的过程,并使用其模拟地下水对皮肤温度的影响。我们发现最大和平均每日土壤温度与地下水深度之间存在极高的负相关性。相反,我们几乎找不到每日最低温度与地下水深度之间的任何关联。数值模拟虽然很简单,但对显示地下水在冬季升高和夏季降低皮肤温度曲线却没有影响曲线形状很有用。我们得出的结论是,浅层地下水通过其在土壤剖面中的独特热特性直接影响皮肤温度,并间接地通过影响土壤水分而间接影响皮肤温度,而土壤水分又对皮肤温度产生许多不同且相互矛盾的影响。这项研究建议建立一个综合的数值模型,以模拟浅层地下水对皮肤温度以及陆地表面不同能量通量的影响。

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