열권, or the "Thermal Zone," refers to a specific area in the atmosphere where temperature changes significantly with altitude. This zone is crucial for understanding weather patterns and climate. It typically extends from the Earth's surface to about 10 kilometers high, where the temperature decreases with altitude. In the context of meteorology, the 열권 plays a vital role in the formation of clouds and precipitation. It is influenced by various factors, including solar radiation and geographical features. Understanding the 열권 helps scientists predict weather changes and study climate variations over time.