Deserts

Introduction

Deserts cover about one-fifth of the Earth's surface and are characterized by extremely low rainfall, typically less than 50 cm (20 inches) annually. They are classified into four main types: hot and dry, semiarid, coastal, and cold. These classifications are based on precipitation, temperature, and location. Desert ecosystems are among the driest on Earth, leading to sparse vegetation and limited biodiversity. Plants and animals in these environments have evolved specialized adaptations for survival. Vegetation often consists of hardy plants with minimal leaves and deep root systems or annual plants that quickly complete their life cycle after rainfall. Animals have adapted to conserve water, often being nocturnal to avoid the intense daytime heat, and may enter dormancy during prolonged dry periods.

Landscape

Desert landscapes are notably diverse, featuring elements like dunes, rock outcrops, and oases. Dunes, shaped by wind, vary in form depending on wind direction and stability. For instance, barchan dunes have a crescent shape with a convex windward side, while seif dunes are long and linear, aligned with dominant winds. Transverse dunes run perpendicular to the wind, and star dunes result from variable wind patterns. Some dunes are stabilized by vegetation or topography, while others are bound by cemented sand grains. Beyond dunes, deserts often include flat, stone-covered plains known as desert pavements. These pavements form as wind erosion removes finer particles, leaving behind larger stones that become stabilized over time through capillary action and mineral precipitation. Other notable desert features include exposed bedrock, dry soils, and formations like alluvial fans and playas. Hamadas are rocky plateaus with wind-eroded sand, while reg or gibber plains are gravel-covered areas with exposed stones. Geologic formations, such as the eroded sandstone outcrops in Algeria’s Tassili Plateau and the canyons of the Colorado Plateau in the U.S., offer insights into the region's erosion and geological history.

Ecosystems and climate

Deserts are categorized into several types based on their climatic and geographical features. Hot and dry deserts, such as those found in North America (like the Mojave and Sonoran Deserts) and Africa, are characterized by high temperatures and low rainfall. Semi-arid deserts, like the Great Basin in North America, receive slightly more rainfall and have less extreme temperatures than hot deserts. Coastal deserts, such as the Atacama in Chile, are influenced by nearby cold ocean currents, leading to cooler temperatures and foggy conditions. Cold deserts, found in places like Antarctica and Greenland, experience significant snowfall and relatively high winter precipitation, with short, mild summers. Desert ecosystems are defined by their extreme aridity and a range of other harsh environmental conditions. Central to all deserts is their characteristic dryness, resulting from minimal rainfall and high evaporation rates. Typically, deserts receive less than 25-30 cm (10-12 inches) of precipitation annually, and some, like the Atacama Desert in Chile, receive as little as 1.5 cm (0.6 inches), or even none at all in some years. Temperature extremes are another defining feature of deserts. During the day, temperatures can soar above 40°C (104°F), while at night, they can plummet below freezing. This drastic fluctuation is due to the lack of atmospheric moisture, which allows for significant heat loss at night. The daytime solar radiation in deserts is considerably higher compared to more humid regions, further exacerbating these temperature swings. Wind velocity in deserts is often high, leading to frequent sandstorms or dust storms that can create large sand dunes. The low humidity during the day and relatively higher humidity at night also characterize desert climates. The soil in deserts tends to be coarse, rocky, and low in nutrients, making it challenging for vegetation to thrive. This soil quality, combined with extreme aridity, results in slow plant growth.

Plant life

Desert plants, or xerophytes, face extreme conditions with limited water and high temperatures. They have evolved various adaptations to survive these challenges. For instance, some use crassulacean acid metabolism (CAM) to open their stomata at night instead of during the day, reducing water loss while still taking in carbon dioxide. Physical adaptations include reduced leaf size or modified stems that store water, as seen in cacti. These plants absorb rain quickly through shallow roots and can store large amounts of water. Additionally, many desert plants have developed strategies to conserve water, such as waxy coatings or hair-like structures on leaves. Reproductive strategies include producing seeds that remain dormant until conditions improve. Some plants, like mesquite, need to pass through an animal's digestive system to germinate. Phreatophytes have deep roots that reach groundwater, providing a steady water supply. Overall, these adaptations enable desert plants to thrive in harsh, arid environments.

Animal life

Desert ecosystems are incredibly harsh, requiring specialized adaptations from their inhabitants to survive. Xerocoles, or desert-adapted animals, have evolved various strategies to handle extreme conditions, with a focus on water conservation and temperature regulation. Birds in deserts use their mobility to their advantage, moving between resources and using thermals to stay cool. Some, like the cream-colored courser, run rather than fly to save energy and blend into their surroundings. The sandgrouse has developed unique feathers to transport water to its chicks. Desert mammals, including endotherms like camels and kangaroo rats, have adapted to manage both heat and hydration. Camels can tolerate significant dehydration and maintain a body temperature close to the desert air temperature, while kangaroo rats produce metabolic water and stay underground to avoid daytime heat. Reptiles and amphibians also exhibit unique adaptations. Reptiles, being ectotherms, avoid daytime heat by sheltering and emerge at night. Amphibians, though generally moisture-dependent, have adapted to desert life by burrowing and remaining dormant until rain triggers their reproductive activities. Invertebrates like beetles and ants have developed hard cuticles to prevent water loss and behavioral strategies to handle extreme temperatures, such as laying eggs underground or capturing moisture from the air.

Test your knowledge

What is a common characteristic of deserts?

3

Which desert type is affected by cold ocean currents, resulting in cooler temperatures?

1