Sahara

The Sahara exhibits great climatic variability within its borders, with two major climatic regimes differentiating along a north-south axis: the desert’s northern latitudes are arid subtropical and have two rainy seasons, while the southern ones, although also arid, are more tropical and have only one rainy season. The southern reaches of the Sahara end in the Sahel, a semiarid buffer zone that separates the desert from the more temperate savanna biomes beyond. A number of other factors affect climatic variability within the Sahara as well: topography does so, as do ocean currents, the latter of which are responsible for the slightly cooler and more humid conditions found on the desert’s western margins. Some scientists estimate that the Sahara became arid about two to three million years ago, while others contend that it happened before this.

In Arabic the Sahara is called Al-Ṣaḥrāʾ al-Kubrā, or “the Great Desert.” The Arabic word ṣaḥrāʾ simply means “desert,” and its plural form, ṣaḥārāʾ, is where the northern African desert gets its Anglicized name. The word ṣaḥrāʾ shares its roots with the Arabic word aṣḥar, which translates to “desert-like” and specifically connotes the yellowish red color that characterizes the Sahara’s sandy expanses.

Though boasting an extremely low primary productivity, the Sahara does manage to support some life. Many of the organisms that can survive have been able to do so with adaptations for arid environments: for example, many herbaceous plants found in the Sahara are ephemerals, meaning that almost all of their life cycle—from germination to seed dispersal—occurs in the two- to three-week period after a heavy rain. Animals such as the desert snail survive by using estivation, a period of dormancy that some animals can enter when encountering extreme environmental stress. Other organisms, although adapted more for a Mediterranean or tropical climate than an arid one, have persisted in the Sahara mostly by sticking to its slightly more hospitable highlands and oases.

People have lived in the Sahara long before recorded history, at certain times in regions that are now too arid for human inhabitance. Archaeological findings indicate that there were once ancient Saharan lakes, upon the shores of which humans lived, hunted, and fished. Even after these lakes ceased to exist, humans survived for centuries in the desert using alternative methods: nomadic pastoralists herded goats, sheep, or camels to whatever pasturage could be found; sedentary agriculturalists, confined to oases, harnessed their limited water resources to grow crops such as date palms and barley; and specialists (for example, blacksmiths) traded wares with their agriculturalist and pastoralist neighbors. Certain groups have long relied on traveling and trading along caravan routes to obtain their livelihood, journeying by camel to oases and population centers all over the Sahara. Modern economic development has disrupted many of these traditional means of subsistence, however, with many desert dwellers seeking more lucrative opportunities in developed regions and oases.

After World War II, prospecting revealed that the Sahara was laden with oil and mineral resources, which have served as a major attractor of international investment since. Oil, natural gas, and coal reserves have been discovered all over northern Africa and particularly have been exploited by various countries, such as Egypt, Libya, and Algeria. Although these industries have introduced potentially high-wage jobs to the Sahara, they are also responsible for the displacement of desert peoples from their traditional modes of existence and have contributed to the increasing overcrowding and poverty in developed regions.