A desert biome is an area that receives less than 25cm (about 9.8 inches) of rainfall a year. Such areas cover about 33% of the land on earth and include areas with a wide variety of land surfaces - from sand or sand dunes to snow, and supporting a correspondingly wide variety of animals and plants. Deserts somtimes expand. This is called desertification.
Deserts are found in many places including: the western part of North America, Western Asia, Central Australia, South America, and south and north Africa. Many, such as the Sahara, are very hot during the day and chilly nights, but there are also deserts such as the Atacama in South America which have below-freezing temperatures throughout the day and night. 
Cold deserts[change | edit source]
There are hot deserts and cold deserts. Cold deserts are covered with snow or ice. Some cold deserts have a short season of above-freezing temperatures. These deserts are called tundra. If the temperature of cold deserts remains below freezing year-round, they are called ice cap.
Cold deserts can be found close to the poles. That is why they are also called polar deserts. Other regions of the world have cold deserts too, for instance high altitude areas like the Himalayas. These are called montane deserts. Antarctica is the world's largest cold desert.
Hot deserts[change | edit source]
Hot deserts are mostly in the subtropics. They can be covered by sand, rock, salt lakes, stony hills and even mountains. Most non-polar deserts are hot in the day and chilly at night. The temperature in the daytime can reach 50 °C or higher in the summer, and dip to 0 °C or lower at nighttime in the winter.
The largest hot desert of the world is the Sahara in North Africa. It is almost as large as Europe or the United States. The Sahara is also the hottest desert in the world.
People sometimes bring water from wet places to hot deserts so plants can grow. This is called irrigation.
Rain[change | edit source]
It does rain in the desert, but not often. In the Atacama Desert it did not rain for 401 years. In other deserts it may rain every year or once every few years. When it rains in a desert, a lot of water may reach the ground in a short time. Some rain passes straight into the dry sand, but the rest may form a temporary river. Wadis, stream channels that are normally dry, can quickly fill after heavy rain, causing a flash flood.
Sandstorm[change | edit source]
Animals and Plants[change | edit source]
There are not many animals in the desert, but some animals are able to survive. They have different ways to survive the intense conditions of the desert. Examples of animals that live in hot deserts are lizards, small rodents, snakes, and camels. Plants and animals in hot deserts must live with very little water.
Xerophytic plants which live in the desert have special adaptations. They may survive by growing roots that are very near the surface to absorb the rain that may fall before it evaporates. Plants such as the cactus have thick, fleshy stems that help them store water.
Animals such as lizards and small rodents often escape the hot rays by digging underground burrows where they live. They only come out at night to search for food. Like the plants, desert animals must live on as little water as possible. Most of the water used by these animals comes from seeds and stems that absorb and hold water. Camels survive in hot deserts by storing water in body fat in their humps. Like other desert animals, the camel loses little water in wastes.
Interesting facts[change | edit source]
- In hot deserts you may see a mirage or fata morgana. A mirage is a trick of the light. It makes you think there is a pool of water in the desert when there is really no water.
References[change | edit source]
- "What Is a Desert?". pubs.usgs.gov. December 18, 2001. http://pubs.usgs.gov/gip/deserts/what/. Retrieved April 9, 2011.
- Pous, Dinorah (2010). Blue Planet: English through Science. North America: McGrawHill. pp. 114 to 115.
- "Desert". Encyclopædia Britannica online. http://www.britannica.com/eb/article-70815/desert. Retrieved 2008-02-09.
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