A desert is a barren area of land where little precipitationoccurs and, consequently, living conditions are hostile for plant and animallife. The lack of vegetation exposes the unprotected surface of the ground to the processes of denudation. About one-third of the landsurface of the world is arid or semi-arid. This includes much of the polar regions where little precipitationoccurs and which are sometimes called polar deserts or "cold deserts".
Characteristics of Deserts
Deserts typically have a number of distinctive features, including:
Low Precipitation: Deserts receive less than 250mm of rainfall annually.
Deserts can be classified into different types based on their geographical location and the prevailing climatic conditions. Some common types of deserts include:
Hot Deserts: These deserts, such as the Sahara in Africa and the Arabian Desert in the Middle East, are characterized by high temperatures and low humidity.
Cold Deserts: Cold deserts, like the Gobi Desert in Asia and the Great Basin Desert in North America, experience extreme temperaturevariations and can be covered in snow during the winter.
Coastal Deserts: Located along the coastlines, these deserts, such as the Atacama Desert in South America, are influenced by cold ocean currents and experience minimal precipitation.
Develop and use models to illustrate that energy at the macroscopic scale can be accounted for as either motions of particles or energy stored in fields.