Desert Habitats, pt.2

Pequop Mountain foothills, Great Basin Desert, Nevada by Matthew Roth, Apr 2016
Big sagebrush, Artimesia tridentata by RCWinton, Aug 2008

There are four major deserts in North America.  The Great Basin runs from central Idaho to northern Arizona.  It is a high altitude plateau, with very cold winters, mild summers, and few plant species characterized by big sagebrush, Artimesia tridentata.

Mohave Desert by Mark Kaletka, May 2012

The Mohave Desert, a small area covering southern Nevada and southeastern California, is known for its cold, rainy winter season resulting in hard freezes leaving little water available.  The Joshua tree, Yucca brevifolia, a yucca variety growing above 3000′, is the tallest plant in the area.

Joshua tree, Yucca brevifolia, by Melissa Delzio, May 2011

The Chihuahuan Desert, covering the high altitudes of northern Mexico ,is subject to hard freezes from arctic winds scouring its surface.  Winter rains occasionally occur supporting a rich diversity of low shrubs and small cacti.

Chihuahuan Desert by Keppet, Feb 2022

The Sonoran Desert, covering southern Arizona and the Baja Peninsula, has high and low altitudes, hot to mild temperatures, and periodic rainfalls.  The winter season, with mild temperatures, does not limit the plant and animal diversity as much as in the other three, colder deserts.  The Sonoran Desert, which includes several habitat types, supports a rich variety of species including 2000+ plants, 350+ birds, 100 reptiles, and 30 native fishes.

Desert plants exhibit many similar features that make them well-adapted to the hot, dry conditions of their native habitat.  Most are succulents, plants with thick, fleshy stems to retain water for use during hot, dry periods.  Plants often have spines in place of leaves to reduce the surface area exposed to wind and heat, greatly reducing water loss from evaporation.  Spines also add a layer of protection to prevent animals from eating the plant.  Stems are green, containing chlorophyll and water, and this is where photosynthesis takes place.  Bloom periods and pollination occur during winter or nighttime when cooler temperatures prevail.

Creosote bush, Larrea tridentata, in flower by Malcom Manners, Apr 2017
Century plant, Agave americana, by J.Maughn, Mar 2020

Several distinctive native species characterize North American deserts including cacti, succulents, and other  plant varieties with spines.  The creosote bush, named for its distinctive antiseptic smell, grows three to nine feet tall and has small yellow flowers.  This plant grows in colonies of cloned bushes which may live for long periods as epitomized by the King Clone of the Mohave Desert, estimated to be about 12,000 years old.  The century plant, another long-lived plant, is a species of agave noted for its large cluster of wide leaves with spiny edges.  The plant may live up to 30 years, but flowers only once, then dies.

Clockwise from top: Prickly pear by Fishfoot, Mar 2018; Prickly pear buds by Diandra Rodriguez, Nov 2011; Prickly pear cacturs in bloom by Stepan Mazurov, May 2009; Prickly pear cactus glochids by Tracie Hall, Nov 2017

Often seen cacti include the prickly pear cactus which is actually a group of several species all native to North America.  Modified stems, called pads, are often mistaken as leaves.  These store water, photosynthesize food and sugars, and produce flowers.  All species grow long, single spines in addition to glochids, clusters of very fine, tiny spines.  Glochids are often not noticeable but can be easily detached if brushed against and once lodged in the skin are painful and difficult to remove.  The saguaro cactus is another common plant.  Its distinctive shape, with a tall central column and “arms” growing at right angles, is easily recognizable as one of the Sonoran Desert’s native species.  It is the largest cactus in North America, growing to over 40′ high, and living 100 years or more.  White, waxy flowers open only at night to attract bats, its preferred pollinator.

Saguaro cactus by Ralph Earlandson, Apr 2017

Many natural history museums have excellent displays of plants and animals from world-wide desert biomes, including one of my favorites, the North American desert display at the Jurica-Suchy Nature Museum.  In my blog next week, I will introduce some of the notable animals and their adaptations to desert life.

Desert Habitat, pt.1

A biome is a type of global habitat characterized by temperature, rainfall, latitude, elevation, and wind pattern.  Plants, which are unable to move about, are used to characterize each type of biome, and are well-adapted to their native habitat.  The desert biome is the driest habitat found on earth.  In a desert, plants are widely spaced and are adapted to life with little or no moisture except for annual periods when brief rains may be heavy, sparse, or not occur at all.  Even within these harsh conditions, plants may be present supporting a rich diversity of species.

Clockwise above: Hidden Valley, Joshua Tree solitude by Don Graham, Apr 2013; Sonoran Desert sunset by Jasper Nance, May 2009; Sonoran Desert layers by Art DiTommaso, Apr 2020; Mohave Desert by Melissa Delzio, May 2011

A common factor of all deserts is the aridity or lack of moisture.  Aridity can be determined by how much water is available in the habitat combined with the rates of evaporation from heat, radiation, and wind exposure.  Another consideration in determining aridity is how much moisture the air can hold.  Neither extremely hot nor extremely cold air easily retains moisture.  Freely running water is only available in the desert for the briefest period of time immediately following a rainfall, a scarce and unpredictable event. 

Deserts form in areas where dry air predominates.  Understanding how weather influences the Earth’s surface helps to identify where to find the world’s desert regions.  At the equator, air is warmed by direct sunlight causing it to rise and absorb large amounts of water from the oceans.  When the warm air mass encounters cooler air at higher altitudes, it spreads out both northward and southward.  Cooler air causes the absorbed moisture to condense into rain in tropical latitudes.  The outward moving air mass, now dryer and cooler, also begins to fall back to the earth’s surface, picking up heat from the sun’s radiation and the hot ground.  Air masses generally descend and move back towards the equator around 30˚ latitude, which is where many deserts occur. 

Rain shadow on leeward side of mountains on Oahu by Loren Javier, Jun 2010
Exploring Greenland’s grass and Dry shrub vegetation by Eugene Kaspersky, Jul 2016

Deserts can also be formed from rain shadows and temperature extremes.  As prevailing winds encounter mountains, air is forced up the windward side and flows down the leeward side.  As air rises, it cools, once again condensing any moisture into rain which falls on the windward side.  Dry air coming over the mountain forms a rain shadow that leaves little moisture for the habitats on the leeward slopes.  Temperature extremes occur in both hot and cold regions.  Dry, hot air descending from the tropics form warm deserts.  Cold, dry air from polar winds form cold deserts such as those found in  Antarctica and Greenland.

Desert temperatures vary widely, both daily and seasonally.  Dry air and cloudless skies allow a maximum amount of solar energy to reach the surface where it is absorbed and converted to heat, raising daytime temperatures dramatically.  At night, air temperatures plummet as solar radiation ceases and heat is quickly wicked away into the cooler atmosphere.  Temperatures may fluctuate as much as 100˚ in a 24-hour period.  Ultraviolet radiation also presents other challenges to living organisms.  Intense sunlight can damage skin cells, degrade retinal tissue, and destroy chlorophyll molecules in plants. 

Rain in the Sonora Desert summer monsoon season by Kevin, Aug 2013
Green Sonoran Desert after brief winter rain by Wayne S. Grazio, Fwb 2017

Deserts experience seasons, just as those found in other biomes.  In desert areas of Arizona, there are five recognized annual seasons.  Spring, February through April, is characterized by mild temperatures and windy days.  It is a dry season as warm winds wick away all exposed moisture.  Summer, in May and June, is hot and dry, with many species remaining dormant to escape the heat.  Summer monsoons, July through mid-September, signals a change in wind direction bringing moister air northward from the tropics.  Frequent thunderstorms occur most years providing a period of replenishment for shrubs and trees.  Autumn, in October and November, returns to warm and dry conditions.  Winter comes in December and January bringing in mild temperatures and the possibility of a few rain showers.

The climate of the world’s deserts makes survival difficult, but many species have adapted to these conditions in some remarkable ways.  Next week, we will investigate the desert regions of North America and their vast diversity of life.

Clockwise above: Blooming hedgehogs by Jasper Nance, Apr 2010; Desert globemallow by Take-A-Hike Arizona, Mar 2009; Desert woollystar, Eriastrum eremicum, Sonoran Desert by SSBiker1, May 2011