Thermodynamic circulation is the simplest form of atmospheric movement. It is an air circulation formed due to uneven cold and heat on the ground. The formation process is as follows: the atmosphere in heated areas expands and rises, forming low air pressure near the ground and high air pressure at high altitudes; on the contrary, in cold areas, an air pressure difference is formed between the horizontal planes near the ground and high altitudes, which promotes the horizontal movement of the atmosphere and forms a thermodynamic circulation at high and low altitudes.
Teachers and students gl Gentle Beauty Geography Teacher
There is an age difference of 10 years, and there is no love during the relationship between teacher and student.
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