Approximately 50% of the heat from the Sun is absorbed at the surface. Consequently, the temperature at the surface may vary considerably according to the day / night cycle, according to weather and particularly according to season. Underground, these temperature changes are blunted and delayed, termed thermal lag. The thermal properties of earth therefore mean that in Winter the temperature below the surface will be higher than the surface air temperature, and conversely in Summer the earth temperature will be lower than the surface air temperature.