High elevations often experience rapid temperature changes.

Rapid temperature changes are common in high-elevation areas due to the thinner atmosphere and lower air density, which cause heat to dissipate quickly. During the day, sunlight can warm the surface rapidly, leading to relatively warmer temperatures, while at night, the lack of atmospheric insulation allows temperatures to drop sharply. These fluctuations can occur within hours, resulting in substantial day-to-night temperature swings. This phenomenon is typical in mountainous regions and has significant effects on local flora and fauna, which must adapt to these dramatic changes in temperature.