A thermal inversion is a meteorological phenomenon where the typical temperature gradient in the atmosphere is reversed, resulting in warmer air trapped above cooler air near the surface. This situation can lead to a variety of effects on air quality and weather patterns, as it inhibits vertical mixing of the atmosphere and can cause pollution to accumulate in the lower layers. Understanding thermal inversions is crucial for grasping concepts like pressure and density variations and their effects on airflow, as well as how they contribute to mountain wave formation.
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