Temperature inversion is formed in the radiative type of weather in the anticyclone weather conditions. In temperature inversion, the temperature of the air increases with height in a certain layer of the air, instead of falling. It is formed in concave relief shape during clear, long and calm nights. Colder air has a higher density therefore, it is kept near the ground, under the warmer air. The purpose of the final seminar work is to analyze the temperature conditions in two separates areas of the study; the bottom of the basin, which lays in the inverse band and the higher laying surroundings above the inversion line. The temperature analysis incorporates four measuring points at various locations for January and April 2018. Based on these, daily and monthly temperature analysis were carried out to determine the characteristics of the temperature inversion according to different weather types and seasons.
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