Wüstenklima

Wüstenklima, also known as arid climate, is characterized by extremely low precipitation. Deserts are typically defined as regions receiving less than 250 millimeters (10 inches) of rainfall annually. This scarcity of water is the defining feature, leading to sparse vegetation and often barren landscapes. Temperatures in desert climates can vary dramatically. Many deserts experience very hot summers with scorching daytime temperatures, which can plummet significantly after sunset due to the lack of cloud cover and humidity to retain heat. Conversely, some deserts are cold deserts, with cold winters and mild summers, but still receive very little precipitation, often in the form of snow. The lack of moisture also means that diurnal temperature ranges (the difference between the highest and lowest temperatures in a single day) are often very large. Winds can be a significant factor in desert environments, contributing to erosion and sand dune formation. The atmospheric conditions, such as clear skies and low humidity, allow for intense solar radiation during the day.