Deserts aren’t extreme because they’re hot, they’re extreme because they’re dry

In this concise explanatory video, Dan Novaes clarifies that deserts are extreme not because of high daytime temperatures but because of their extreme dryness. He explains that atmospheric moisture acts like a blanket that retains heat; deserts lack this moisture, so after sunset heat radiates away rapidly, leading to sharp nighttime cooling. Clear skies, common in deserts, further accelerate heat loss because clouds normally trap infrared radiation. The ground itself contributes: dry sand has low heat capacity and releases stored heat quickly, unlike moist soils. Novaes also notes that Antarctica qualifies as the world’s largest desert due to its very low precipitation, illustrating that deserts can be cold as well as hot. The overall message is that the lack of water—both in the air and in the ground—creates large diurnal temperature swings, making desert environments feel especially intense.











