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Past Surface Temperatures Reconstructed by Inversion of the Measured Borehole Temperature-Depth Profiles in Rock

机译:通过反演岩石中钻孔温度-深度剖面重建过去的地表温度

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The measured temperature-depth profiles in boreholes are proxy climate indicators. The climatic temperature signal at the surface penetrates in the rock thickness and disturbs the steady-state temperature of the Earth. The measured temperature-depth profile can be so-called the re-determination condition to solve the inverse problem for the thermal diffusivity equation, and retrieve the past surface temperature history. We study properties of solution for this problem. We derive that the solution is not unique. However, there were done numerous past surface temperature reconstructions. We show that it is needed to take into account some a priori data to determine past temperatures correctly.
机译:钻孔中测得的温度-深度剖面是替代气候指标。地表的气候温度信号穿透了岩石厚度,并扰乱了地球的稳态温度。测得的温度-深度轮廓可以称为重新确定条件,以解决热扩散方程的反问题,并获取过去的表面温度历史记录。我们研究该问题的解决方案的性质。我们得出的解决方案不是唯一的。但是,过去进行了大量的表面温度重建。我们表明,需要考虑一些先验数据来正确确定过去的温度。

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