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Ground Surface Temperature History in Poland in the 16th–20th Centuries Derived from the Inversion of Geothermal Profiles

机译:地热剖面反演推导的16至20世纪波兰地表温度历史

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摘要

Ground Surface Temperature (GST) history in Poland was derived from the inversion of temperature-depth profiles in over 20 wells. Temperature histories for the period 1500 A.D. through 1977 A.D. agree well with the instrumental record of the surface-air temperature available for the last two centuries. A statistical correlation of the reconstructed histories (from the well temperature data) with the instrumental record (air temperature) from the homogeneous Warsaw series is high (>0.8). Functional space inversion (FSI) of the temperature data with depth shows that beginning in the early 19th century, temperatures warmed by 0.9 ± 0.1°C following a long period of colder climate before. The last number could be a minimal as higher warming was calculated using a simple model based on surface temperature for the observational period (homogenized Warsaw surface temperature series, Lorenc, 2000) and POM (pre-observational mean; Harris and Chapman, 1998) of −1.53oC below the 1951–1980 mean temperature level.
机译:波兰的地表温度(GST)历史源自对20多个井的温度-深度剖面的反演。从公元1500年到1977年的温度历史与过去两个世纪以来可用的地面空气温度的仪器记录非常吻合。重构历史(来自井温度数据)与均质华沙系列的仪器记录(气温)的统计相关性很高(> 0.8)。具有深度的温度数据的函数空间反演(FSI)表明,从19世纪初开始,经过很长时间的较冷气候,温度升高了0.9±0.1°C。最后一个数字可能是最小的,因为使用简单模型基于观测期的地面温度(均化的华沙表面温度系列,Lorenc,2000年)和POM(观测前平均值; Harris和Chapman,1998年)来计算较高的变暖。低于1951–1980年平均温度水平−1.53o C。

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