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Prediction of soil frost penetration depth in northwest of Iran using air freezing indices

机译:利用空气冻结指数预测伊朗西北部土壤霜的渗透深度

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Information about soil frost penetration depth can be effective in finding appropriate solutions to reduce the agricultural crop damage, transportations, and building facilities. Amongst proper methods to achieve this information are the statistical and empirical models capable of estimating soil frost penetration depth. Therefore, the main objective of this research is to calculate soil frost penetration depth in northwest of Iran during the year 2007-2008 to validate two different models accuracy. To do so, the relationship between air and soil temperature in different depths (5-10-20-30-50-100 cm) at three times of the day (3, 9, and 15 GMT) for 14 weather stations over 7 provinces was analyzed using linear regression. Then, two different air freezing indices (AFIs) including Norwegian and Finn AFI was implemented. Finally, the frost penetration depth was calculated by McKeown method and the accuracy of models determined by actual soil frost penetration depth. The results demonstrated that there is a significant correlation between air and soil depth temperature in all studied stations up to the 30 cm under the surface. Also, according to the results, Norwegian index can be effectively used for determination of soil frost depth penetration and the correlation coefficient between actual and estimated soil frost penetration depth is r = 0.92 while the Finn index overestimates the frost depth in all stations with correlation coefficient r = 0.70.
机译:有关土壤霜渗透深度的信息可以有效地找到适当的解决方案,以减少对农作物的损害,运输和建筑设施。获得该信息的适当方法之一是能够估算土壤霜渗透深度的统计和经验模型。因此,本研究的主要目的是计算伊朗西北部2007-2008年间的土壤霜渗透深度,以验证两种不同模型的准确性。为此,对于7个省的14个气象站,一天三遍(3、9和15 GMT)不同深度(5-10-20-30-50-100 cm)的空气和土壤温度之间的关系使用线性回归分析。然后,实施了两个不同的空气冻结指数(AFI),包括挪威和芬兰的AFI。最后,通过McKeown方法计算了霜冻渗透深度,并通过实际的土壤霜冻渗透深度确定了模型的准确性。结果表明,在所有研究到的地面以下30厘米以下的站点中,空气和土壤深度温度之间都存在显着的相关性。同样,根据结果,挪威指数可以有效地用于确定土壤霜冻深度的渗透,实际和估计的霜冻渗透深度之间的相关系数为r = 0.92,而Finn指数则通过相关系数高估了所有站点的霜冻深度r = 0.70。

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