On the other hand, deserts are characterized by clear skies with little cloud cover. This allows for efficient heat loss through radiation at night. As the sun sets, the sand rapidly loses its heat back into the atmosphere through infrared radiation. Since there is minimal atmospheric moisture or cloud cover to trap the heat, the temperature drops drastically. The absence of vegetation and other heat-absorbing objects in deserts further contributes to the rapid heat loss.
This diurnal temperature variation in deserts can be substantial. During the day, desert sand temperatures can reach as high as 60°C (140°F) or even higher, while at night, they can drop to freezing temperatures or below, sometimes reaching as low as -18°C (0°F). This significant temperature fluctuation is a distinctive feature of desert environments.