Abstract
Procedural questions related to the construction of mathematical models that establish a quantitative relationship between certain characteristics of the temperature field and the indicator of damping of the pulse electromagnetic field in a layer of the annual temperature fluctuations of built-up areas of the cryolithic zone of Yakutia are considered. Recommendations are given for practical application of the mathematical models based on an analysis of the errors that arise when calculating the temperature of frozen ground found with the use of the models.
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