Temperature inversion occurs when warm air traps cooler air near the surface, disrupting normal temperature patterns. It affects air quality, weather, agriculture, and transport. Understanding its causes and impacts is vital for effective environmental and safety planning.
theIASHub | 17 Jul, 2025
Temperature inversion refers to a meteorological phenomenon in which the temperature of the atmosphere increases with altitude, contrary to the normal decrease in temperature with height. In this case, a layer of warm air is trapped above a layer of cooler air near the Earth's surface, leading to an inversion of the usual temperature profile. Temperature inversions can occur in various atmospheric conditions and have both natural and human-induced causes. They can have significant impacts on weather, air quality, and human activities.
Understanding temperature inversions and their causes and impacts is crucial for various sectors, including meteorology, air quality management, agriculture, and transportation. Monitoring and predicting temperature inversions can help mitigate their adverse effects and improve planning and decision-making processes related to weather and environmental conditions.
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