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Predicting Daily Mean Soil Temperature from Daily Mean Air Temperature in Four Northern Hardwood Forest Stands

机译:从北部四个阔叶林林分的日平均气温预测日平均土壤温度

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Soil temperature is very important in regulating ecosystem processes, yet it is often difficult and costly to measure. Most models that have endeavored to predict soil temperature have either a long time step or several complicated independent variables. Daily mean air and soil temperatures were measured from 1989-1997 in four northern hardwood sites along a 500 km latitudinal gradient in Michigan. These data were used to derive a simple method to predict daily mean soil temperature (depth of 15 cm)using the daily mean air temperature from the previous day and a cosine function of Julian date (R-2=0.93-0.96;SEM=0.98-1.40 deg C).
机译:土壤温度在调节生态系统过程中非常重要,但测量通常很困难且成本很高。大多数努力预测土壤温度的模型要么时间较长,要么具有多个复杂的自变量。 1989年至1997年期间,在密歇根州北部沿500 km的纬度梯度测量了四个北部硬木站点的每日平均空气和土壤温度。这些数据被用来推导一种简单的方法来预测日平均土壤温度(深度为15 cm),该方法使用前一天的日平均气温和朱利安日期的余弦函数(R-2 = 0.93-0.96; SEM = 0.98) -1.40摄氏度)。

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