What comes to your mind when you hear the mention of the word ‘desert’? Probably a dry area with extremely hot temperatures, right?
Well, while it’s true that all deserts are dry, they necessarily don’t have to be hot. We have cold deserts, and a perfect case in point is the Gobi desert in Asia.
But then, regardless of the region and whether it falls in the cold or hot category, any desert is usually cold at night and receives very little rainfall. However, despite the minimal precipitation, deserts produce plants that have adapted to such living conditions.
Several things make up a desert ecosystem. Among those are:
The ecosystem is dependent upon the type of desert (whether temperate deserts, also referred to as cold deserts, or hot, now the subtropical deserts).
Hot deserts and cold deserts have different kinds of ecosystems. However, despite being very different, the two kinds of deserts have a few similarities.
Similarities of temperate and subtropical deserts:
- Both get fewer than 10 inches of rain annually.
- Dry air is found in both kinds of biomes.
- Both have harsh living conditions that impact people or animals living there.
- Plants have adapted to having less water and harsher temperatures.
- Animals have adapted to the conditions as far as energy, food consumption, and when to get out and be active.
In general, deserts are made up of a number of abiotic components, including sand, the lack of moisture, extreme hot or cold temperatures, and basically anything else that makes up an ecosystem that isn’t alive. However, there are also a number of biotic factors that affect deserts, which include living things, such as plants and animals.
Factors falling under the abiotic components include climate, location, temperature, and precipitation.
Let’s take a close examination of each of these elements;
The climate of temperate deserts differs from that of subtropical deserts.
Antarctica is an example of a temperate desert. The temperatures are actually so cold, in fact, too cold, that they could even lead to the death of humans.
But we still have animals living in these deserts. To survive, these animals have adapted with the passage of time. The ways they have done this is by adding extra layers of fat or needing less food and energy in order to survive.
These deserts are too hot for many plants and animals to handle. The animals who call these deserts home have adapted to having less water. Because it is so hot during the day, they have become nocturnal, getting out during the night when it is cooler and easier to maneuver without getting overheated.
But, because the nights are cold, they have had to become accustomed to the colder nights. Plants have had to adjust to having less water, so they are sparse and often close to the ground.
The formation of deserts can be attributed to two primary factors: rain shadows created by mountains and the extensive circulation of global winds.
As moisture-laden air ascends the slopes of mountains, it cools and releases precipitation on the windward side of the mountain. In the case of substantial mountain ranges, minimal moisture reaches the leeward side.
Consequently, deserts are frequently located in close proximity to mountainous regions, including:
- The Caucasus Mountains in Asia, where the Karakum and Kyzyl Kum deserts are;
- The Atacama Desert, which is partly caused by the Andes Mountains in Chile;
- Parts of California, where the Santa Cruz mountains are;
- The Sahara desert is affected by a number of different mountain ranges.
Global wind patterns, which are complicated, play a significant role in where deserts are located. Winds that circle the globe are the result of the difference between warmer equatorial temperatures as well as the polar temperatures that are cooler.
After the air has been warmed at the equator, it moves upward. It then moves toward the North Pole and toward the South Pole, where it loses moisture, cools off, and then sinks before returning to the equator. Therefore, stable wind patterns and shifting global patterns can contribute to where a desert is.
The passage of time greatly influences where and how deserts form. As time has passed, the locations of deserts have moved through the passage of geologic time. This change has been the result of the uplifting of mountain ranges and continental drift.
The horse latitudes are where more deserts are situated, which is generally straddling the Tropic of Capricorn and the Tropic of Cancer, which falls between 15 and 30 degrees to the equator’s north.
There are geologically ancient deserts, such as the Sahara Desert in northern Africa, which is 65 million years old, or the Kalahari in central Africa. In North America, three of the four major deserts are within a geological region called the Range Province and the Basin, which falls between the Sierra Nevadas and the Rocky Mountains, and then extending into the state of Sonora in Mexico.
The forces of erosion thousands of years past shaped the desert landscapes during heavy rainfall. The rocky mountain slopes and hillsides caught the rain, which picked up loose sediment, sand, cobbles, and boulders and then moved them.
As gravity caused the water to be carried downhill, sediment was moved down to the basin. At the bottom of the mountain, the water spread out across a broad area where the mouths of canyons were widened.
The temperature of a given desert will vary due to its geographic location. However, a characteristic of all deserts is the dryness. Heat is reflected by water vapor, which is either in the form of cloud cover or humidity, resulting in a cooling effect. Because of the reactions and the characteristics, deserts experience extreme temperatures, regardless of whether it is heat or cold.
The temperature fluctuations can result in other effects. Cool air sinks, and warm air rises, so the fast changes in temperatures cause the air to move fast from one place to another. Because of that, deserts are windy, and those conditions contribute to evaporation.
Roughly 90% of the sunlight is permitted through clear, arid air, a significant contrast to the approximately 40% of sunlight that typically penetrates the atmosphere in humid climates. This surplus sunlight includes ultraviolet radiation, which can pose substantial risks to plants, animals, and humans, potentially causing significant harm.
The desert environment has unpredictable and uneven precipitation that it does receive, although that precipitation is minimal in nature. Precipitation amounts can vary from year to year.
Some years, it may seem as though the desert has gotten more rainfall than usual, but most years have very little rainfall. There can actually be entire years that the desert doesn’t see a drop of rain.
Biotic components of a desert, as already stated, include the living organisms. This means there are two of them: plant life and animal life.
Water is essential everywhere and for every living thing. And it is, of course, extremely important in the desert. Because of the lack of water, plants growing in deserts, also known as Xerophytes, have made major adaptations.
- The seeds of annual plants stay dormant until a time when there is adequate rainfall available to support a young plant.
- Cacti and other succulent plants store water in their spines, which are residual leaves. The stem is where photosynthesis takes place, and the stem has pleats that are able to expand fast when rain falls.
- Evergreens have way cuticles and sunken stomata on shrubs that help hold water and prevent it from escaping. As an example, the holly plant’s leaves are held at 70-degree angles, so the sun only hits its sides. When the sun sinks low in the sky, the entire leaf is exposed. A fine salt covering is on the leaves, and that helps reflect the sun off of the plant.
More than a fifth of the earth’s land is comprised of deserts. The lack of water can create a survival problem for any humans, animals, plants, or other organisms. Besides the low rainfall, deserts experience a high amount of water loss from evaporation from the ground and through the transpiration of plants.
Evapotranspiration is from the combination of evaporation and transpiration. Potential evapotranspiration is how much water that would be lost by transpiration and evaporation if they were possible. Scientists measure this amount under controlled conditions with a large pan of water.
The soil in the desert is known for its coarseness, which permits the little moisture that is in it to pass through quickly, which means it is not as available for plants. Salts accumulate as a result of the high evaporation rate. The soil becomes alkaline and limits plant growth, which is also known as primary productivity.
Because of the entire process required to maintain life in the desert, the size of individual animals and that of the populations is limited. The extremes of heat and aridity that result in deserts are one of the most fragile ecosystems in the world.
Visitors to the desert should also take the proper precautions to protect themselves, as the environment is much different than that of any other location.
Despite common beliefs that things can’t live in the desert, there are a number of creatures that have learned to survive on the distinctive plant life and in difficult conditions.
- Large mammals like camels make their homes in the desert and are suited to travel long periods of time without water. Lions live in the deserts of Africa, although they are endangered due to changing weather patterns and the presence of humans.
- Small rodents find homes in the desert, with variations from gerbils to hedgehogs. Larger hyenas and jackals are also often found in deserts.
- Lizards and snakes are particularly suited to the dry, hot climate of the desert, as are amphibious creatures like a number of toads and salamanders.
Importance of Desert Ecosystem
Despite the profound temperature extremities, the desert biome is very important to this earth. Deserts can be found on every single continent, and even though they lack water, they play an essential role in helping animals, humans, and the environment.
1. Flora & Fauna
Deserts are home to a vast array of unique plants and animals that have adapted to their harsh habitats. They are home to various livestock, such as camels, goats, and antelope, that provide food and livelihood for people.
Desert shrubs and trees that produce fruit such as dates, one of the oldest cultivated foods in the world dating back to biblical times, and figs and olives are an important food source in North Africa and the Middle East.
Besides adding to the Earth’s biodiversity, many of these plants and animals benefit humans. Domesticated camels in the deserts of Asia and North Africa have been reliable pack animals for thousands of years. If deserts disappear, many insects and animal species will also disappear. Many biotic factors count on deserts for food, water, and shelter.
2. Mineral Resources
There are 15 mineral deposit types on our planet, and 13 of them are found in deserts. Some important minerals form and concentrate in the dry conditions of deserts.
Gypsum, borates, nitrates, potassium, and other salts build up in deserts when water carrying these minerals evaporates. The extraction of important minerals from desert regions has become easier due to minimal vegetation.
According to United Nations statistics, over 50% of world copper comes from deserts in Mexico, Australia, and Chile. Other minerals and metals like bauxite, gold, and diamonds can be found in large quantities in the deserts of China, the United States, and Namibia. Desert regions also hold 75% of known oil reserves in the world.
3. Carbon Sinks
According to an article in Science Daily, desert sands are an important carbon sink on Earth. Scientists discovered that cyanobacteria living in the sands of the Kalahari Desert of Botswana help gather and store carbon dioxide from the air.
These drought-resistant bacteria can fix atmospheric carbon dioxide, and together, they add significant quantities of organic matter to the nutrient-deficient sands. Since carbon dioxide is one of the prime causes of global warming, these desert sands may play a critical role in preventing additional carbon dioxide from entering the atmosphere.
4. Archeological Discoveries
Arid conditions are ideal for preserving human artifacts and remains. Present-day archaeologists came to know about ancient civilizations from mummified human remains found in countries like Peru, China, and Egypt have taught.
For example, in March 2010, the New York Times reported that scientists working in the middle of a terrifying desert north of Tibet, in western China, discovered a 4,000-year-old cemetery of 200 corpses with European facial features.
The cemetery lies in what is now China’s northwest autonomous region of Xinjiang, yet the people there have European features, with brown hair and long noses. Discoveries such as these help shape the modern understanding of how our societies first formed.
5. Leisure and Tourism
Deserts hold a unique allure, drawing in millions of visitors annually. The deserts of the Middle East and North Africa, for instance, showcase iconic attractions like Egypt’s Great Pyramids in Giza, Jordan’s ancient city of Petra, the historical remnants of Carthage, and numerous other remarkably well-preserved archaeological ruins from the past.
In the United States, the deserts of modern New Mexico, Utah, and Arizona were once home to the Chaco culture, as well as indigenous Pueblo peoples such as the Anasazi and Hohokum, leaving behind a rich tapestry of historical significance and cultural heritage.
The Anasazi houses at Mesa Verde are an incredible site, as is the Casa Grande monument in Arizona, built by the Hohokum Culture. In South America, there are many sites and artifacts recovered from the Atacama.
Desert plants have adapted special properties that help them survive in harsh desert climates. According to scientists, certain chemically-based adaptations can have medical applications in humans. According to a UN report on the global outlook of deserts, a recent survey of plants in Israel’s Negev desert found plants that could be used to fight malaria.