Desert climate
Desert Climate
Desert Climate (pronunciation: /ˈdezərt ˈklaɪmɪt/) is a type of climate that is characterized by extremely high temperatures and very low precipitation. The term "desert climate" is derived from the Latin word "desertus" which means "abandoned" and the Greek word "klima" which means "inclination, slope".
Characteristics
The main characteristics of a desert climate include high temperatures, low precipitation, and high evaporation rates. These climates are typically found in regions that are located in the interior of continents, away from the moderating influence of large bodies of water.
Types of Desert Climates
There are two main types of desert climates: hot desert climates and cold desert climates. Hot desert climates are typically found in tropical and subtropical regions, while cold desert climates are typically found in temperate regions.
Flora and Fauna
The flora and fauna in desert climates have adapted to survive in these harsh conditions. Plants such as cacti and succulents have developed adaptations to conserve water, while animals such as camels and fennec foxes have developed adaptations to withstand the extreme temperatures.
Human Adaptation
Humans have also adapted to live in desert climates. These adaptations include the construction of adobe buildings, the cultivation of irrigated crops, and the domestication of animals such as camels and goats.
See Also
External links
- Medical encyclopedia article on Desert climate
- Wikipedia's article - Desert climate
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