What Is a Desert? The Driest Places on Earth
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What Is a Desert? The Driest Places on Earth

A desert is a region with very low precipitation (less than 250mm/year). They cover about a third of Earth's land and include hot deserts like the Sahara and cold ones like Antarctica.

Geography Worlds
March 26, 2026
6 min read

Deserts are some of Earth's most extreme environments — places where life persists despite minimal water. They cover about a third of our planet's land surface and come in surprising variety. Hot sandy deserts like the Sahara are familiar, but deserts also include vast cold regions like Antarctica and rocky landscapes like the Atacama. All share one defining feature: extreme dryness.

The Short Answer

A desert is a region that receives less than 250 mm (10 inches) of precipitation per year, making it arid (dry). Deserts come in different types: hot deserts (Sahara, Arabian), cold deserts (Antarctica, Gobi), coastal deserts (Atacama, Namib), and rain shadow deserts (Death Valley, Mojave). They cover about 33% of Earth's land surface and support unique ecosystems adapted to extreme dryness.

What Makes a Desert

The defining feature is aridity:

  • Less than 250 mm/year: The standard definition.
  • Some are extreme: Atacama has parts with no measurable rain in centuries.
  • Variability: Some deserts get years without rain, then a downpour.
  • High evaporation: Combined with low rainfall = water scarcity.
  • Climate scientists also look at evaporation rates.

Types of Deserts

  • Hot deserts: Sahara, Arabian, Australian Outback, Mexican deserts. Hot day temperatures.
  • Cold deserts: Antarctica, Gobi, parts of US Great Basin. Very cold winters.
  • Coastal deserts: Atacama (Chile), Namib (Namibia). Cold ocean currents bring fog but little rain.
  • Rain shadow deserts: Death Valley, Mojave. Mountains block rain.
  • Polar deserts: Antarctica, parts of Arctic. Extreme cold prevents precipitation.

Largest Deserts

  • Antarctica: 14 million km² — the largest desert (cold).
  • Arctic: 13.7 million km² (cold).
  • Sahara: 9.2 million km² (hot, largest hot desert).
  • Arabian: 2.3 million km².
  • Gobi: 1.3 million km².
  • Kalahari: 900,000 km².
  • Patagonian: 670,000 km².
  • Great Basin (USA): 492,000 km².

The Sahara

The famous hot desert:

  • 9.2 million km² — about the size of the USA
  • Crosses 11 countries
  • Highest recorded temperature: 58°C (137°F)
  • Was once tropical 6,000 years ago
  • Massive dunes called "ergs"
  • Hosts ~2.5 million people

The Atacama

Driest non-polar desert:

  • In northern Chile
  • Some weather stations have never recorded rain
  • Average rainfall: less than 1 mm/year
  • Caused by cold Pacific currents and Andes rain shadow
  • Lakes are dry salt flats (salar)
  • Mars-like landscape used for rover testing

Antarctica

The world's largest desert:

  • Coldest place on Earth (lowest -89°C recorded)
  • 98% ice-covered
  • Very low precipitation overall
  • 14 million km² of mostly continent
  • Surrounded by Southern Ocean
  • No permanent residents (just researchers)

Desert Climate

Common features:

  • Extreme daily temperature variation
  • Hot days, cold nights
  • Low humidity
  • Strong winds
  • Intense solar radiation
  • Periodic dust storms
  • Most live in extreme conditions

Why Deserts Form

Several causes:

  • Subtropical high pressure: Air sinks at ~30° latitude, becoming dry. Sahara, Arabian, Australian deserts.
  • Rain shadow: Mountains block precipitation. Death Valley behind Sierra Nevada.
  • Coastal currents: Cold ocean water makes dry air. Atacama and Namib.
  • Inland location: Far from oceans. Gobi.
  • Polar regions: Cold air holds little moisture. Antarctica.

Desert Landscapes

Surprising variety:

  • Sand dunes (ergs): Like Arabian and Saharan dunes.
  • Rocky deserts (reg): Stones and pavement, common in Sahara.
  • Salt flats: Like Salar de Uyuni in Bolivia.
  • Canyons and badlands: Eroded landscapes.
  • Mesas and plateaus: Flat-topped formations.
  • Sand seas: Vast dune fields.

Desert Life

Animals and plants adapt:

  • Camels: Iconic desert mammals.
  • Lizards, snakes, scorpions: Cold-blooded adapted to extreme temperatures.
  • Cacti, succulents: Water-storing plants.
  • Kangaroo rats, gerbils: Get water from food.
  • Hyenas, foxes: Nocturnal predators.
  • Migratory birds: Use deserts seasonally.

How Cacti Survive

Adaptations include:

  • Water storage in stems
  • Reduced leaves (spines) to minimize evaporation
  • CAM photosynthesis (open stomata at night)
  • Deep or wide root systems
  • Thick waxy skin
  • Can survive years of drought

Human Populations

People live in deserts:

  • Bedouin tribes in Arabian and Sahara
  • Tuareg in North African deserts
  • Aboriginal Australians in Outback
  • Mongolian and Chinese peoples in Gobi
  • San (Bushmen) in Kalahari
  • Modern cities: Las Vegas, Phoenix, Dubai, Riyadh, etc.

Famous Desert Cities

  • Las Vegas (USA): 650,000+ in Mojave Desert.
  • Phoenix (USA): 1.7+ million in Sonoran Desert.
  • Cairo (Egypt): 20+ million on Saharan edge.
  • Dubai (UAE): 3+ million in Arabian Desert.
  • Lima (Peru): 10+ million on Atacama edge.
  • Tehran (Iran): 9+ million in arid region.

Desert Climate Change

Deserts and warming:

  • Many deserts expanding
  • "Desertification" affects more land
  • Sahel region of Africa drying
  • Less reliable monsoon affecting Indian agriculture
  • Water resources increasingly stressed
  • Climate refugees increasing

Water in Deserts

Sources of water:

  • Oases: Underground water reaching the surface.
  • Wadis/arroyos: Dry riverbeds; flow only during rains.
  • Springs: Various sources of underground water.
  • Underground aquifers: Some massive (Nubian sandstone aquifer).
  • Mountain glaciers: Provide water for desert valleys.
  • Desalination: Modern technology converts seawater.

Famous Oases

  • Siwa Oasis (Egypt): Historic Saharan oasis.
  • Al Hasa Oasis (Saudi Arabia): Largest in the world.
  • Las Vegas Springs: Original Mojave oasis.
  • Liwa Oasis (UAE): Source for many tribes.
  • Damascus (Syria): Originally oasis-based city.
  • Many were strategic for trade routes.

Desert Trade Routes

Historic desert commerce:

  • Trans-Saharan caravan routes
  • Silk Road through Asian deserts
  • Frankincense trail in Arabia
  • Camel caravans moved goods
  • Major civilizations depended on these
  • Sea routes eventually replaced most

Desert Tourism

Modern attractions:

  • Safari expeditions in Sahara, Kalahari
  • Adventure tourism in many deserts
  • Photographing dunes and rock formations
  • Stargazing (deserts have darkest skies)
  • Cultural tourism with indigenous peoples
  • Visiting historic oases and ruins

Desert Records

  • Driest: Atacama Desert.
  • Hottest: Death Valley (56.7°C recorded).
  • Largest sand dune: Big Daddy, Namib (380 m tall).
  • Largest desert (cold): Antarctica.
  • Largest hot desert: Sahara.
  • Oldest: Namib, possibly 55 million years old.

Why Deserts Matter

Importance beyond their barren appearance:

  • Massive solar energy potential
  • Important mineral deposits
  • Unique ecosystems
  • Climate indicators
  • Indigenous cultural heritage
  • Geological and astronomical research sites
  • Tourism economic value

Key Facts

  • A desert receives less than 250 mm of rain per year.
  • Antarctica is the world's largest desert.
  • Sahara is the largest hot desert.
  • Atacama is one of the driest places on Earth.
  • Deserts cover about 33% of Earth's land.

Fun Facts

  • Antarctica is technically a desert despite being covered in ice.
  • The Sahara was green and lush 6,000 years ago.
  • The Atacama has weather stations that have never recorded rain.
  • Death Valley reached 56.7°C in 1913 — the hottest recorded temperature.
  • Some desert plants can wait years for rain to germinate.

Desert Animals

Desert animals show equally remarkable adaptations. Camels can go weeks without water, stored in their bodies in various forms. Kangaroo rats never need to drink water, getting moisture from food. Fennec foxes have huge ears for heat dissipation. Sidewinder snakes move sideways to minimize hot sand contact. Many desert animals are nocturnal to avoid daytime heat. Some can hibernate during dry periods. Lizards regulate temperature behaviorally. Desert birds may travel hundreds of kilometers daily to find water. Despite the harshness, deserts host surprising diversity. Each species' adaptations reveal evolution's power to make life possible even in extreme environments.

Desert Plants

Desert plants have evolved remarkable adaptations. Cacti store water in their stems, have spines instead of leaves to minimize evaporation, and use CAM photosynthesis (opening stomata at night). Mesquite trees have roots reaching down 50 meters to access deep groundwater. Desert wildflowers may wait years for sufficient rain to germinate. Some plants concentrate salts in leaves. Others have hairy leaves that reflect heat. Saguaro cacti can live 150+ years and weigh several tons. Date palms thrive in oases. Each adaptation evolved over thousands or millions of years. Together, these strategies enable surprising diversity of plant life in some of Earth's harshest environments.

Desert Survival

Surviving in deserts requires understanding. Water is the critical resource — humans need 4+ liters daily in hot deserts. Shade and timing exposure to avoid midday sun is essential. Knowing terrain helps locate water sources at oases, hidden springs, or wadis after rain. Indigenous peoples have developed extensive survival knowledge. Modern desert travelers use GPS, satellite communication, and water purification. Tales of survival demonstrate human resilience: people have survived weeks without food but typically die within days without water. Desert military operations, search-and-rescue, and adventure activities all require specialized training and equipment.

Future of Deserts

Climate change is reshaping deserts. Some are expanding (the Sahel region of Africa, parts of the American Southwest). Some are becoming more variable in precipitation patterns. The Atacama may see unusual rainfall events. Population growth in desert regions strains water resources. Massive water projects (Saudi pivot irrigation, Israeli desalination) attempt to support agriculture and cities. Some regions face permanent depopulation. Conversely, some desert regions attract climate refugees from elsewhere. The 21st century will see major changes in desert geography, demography, and ecosystem services.

The Bottom Line

A desert is a region defined by extreme aridity — less than 250 mm of precipitation per year. Despite this minimal water, deserts support remarkable biodiversity and human populations. They come in surprising variety, from hot Saharan dunes to cold Antarctic plains. Deserts cover a third of Earth's land, contain valuable resources, host indigenous peoples with rich cultures, and serve as windows into Earth's climate history and processes. Climate change is reshaping deserts in significant ways across the globe.