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In this paper we present the results of monitoring of temperatures in the air, soil and a borehole V-8/86 at\udMalence near Kostanjevica in the southeast Slovenia. The results include the temperatures measured in the period\udfrom year 2011 to 2015. Highlights of the paper are mainly on the inflence of heavy rainfall on temperatures in\udthe upper parts of the shallow subsurface, on understanding how the heat transfers between air and soil and in\uddetermination of the warming rate in the shallow subsurface with the assumption that conduction is the prevalent\udmechanism of heat transfer within the rock. The analysis has shown that heavy rainfall has a greater impact at\uddepth of 1 m in the borehole than at 1 m in the soil, since the sensor at 1 m in the borehole is actually still in the\udair (inside the borehole) so the rainwater and consequently the air temperature change can reach it faster than the\udrainwater can infitrate through soil to depth of 1 m. During infitration the rainwater’s temperature interact with\udthe soil temperature and the change between the rainwater and soil temperatures is no longer evident at 1 m depth\udin the soil. Based on the measured temperatures from years 2014 and 2015 the rate of warming at the depth of 40\udm is 0.011 °C/yr. While analysing the temperature-depth profie of daily means of temperature on the 15th day of\udeach month, we concluded that the inflence of seasons can be tracked down to depth of 20 m. At the depth of 20 m\udtemperatures vary within 0.04 °C (2015). The assumption that the conduction is the prevalent mechanism of heat\udtransfer is reasonable, because the theoretical values do not differ much from the measured ones (within 5 %)

Investigations of the air – ground temperature coupling atlocation of the Malence borehole near Kostanjevica, SE Slovenia