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High Quality Content by WIKIPEDIA articles! High Quality Content by WIKIPEDIA articles! High Quality Content by WIKIPEDIA articles! Thermal lows are non-frontal low-pressure areas that occur over the continents in the subtropics such as near the Sonoran Desert, the Mexican plateau, Sahara, South America over northwest Argentina, Australia, the Iberian peninsula, and Tibetan plateau during the warm season as the result of intense heating when compared to their surrounding environments. Over land, intense, rapid solar heating of the lower layers of air creates hot air, which is less dense than surrounding cooler air. This, combined with the rising of the hot air, results in the formation of a low pressure area.