The “Deserts” of Colombia, Most of Which Are Relatively Humid, and the “Problem Climate” of the Guajira Peninsula
Given that Colombia is usually considered the world’s rainiest country, with roughly 3,240 millimeters (128 inches) of average annual precipitation, I was surprised to find tourism firms advertising visits to the “Deserts of Colombia.” To be sure, Colombia does have one true desert, as defined by climatological criteria. La Guajira Desert, in the northern Guajira Peninsula of far northern Colombia, receives some 200 to 300 mm of precipitation annually. As “deserts” are often defined as areas that get less than 250 mm (9.8 inches), this area qualifies. Its cactus-filled landscapes certainly match a common American perception of what constitutes a “desert.”
As the precipitation map posted below shows, no other part of Colombia climatologically qualifies as a desert environment. The drier areas of the country, depicted in shades of light brown on map below, receive as much as 1000 mm (39 inches) of rainfall annually, a relatively high number. The brown areas around and to the northeast of Bogota are relatively wet, as they sit at high elevations and thus have cool climates with low rates of evaporation. Where then are Colombia’s other “deserts”?

This key issue here is how the English word “desert” is defined. Historically, it could refer to any uninhabited or “deserted” place, regardless of rainfall. It later came to refer to any arid or semi-arid area that had few trees. In the early and mid-19th century, the Great Plains of the United States was often mapped as “the Great American Desert,” but it is now never regarded in such a manner. In popular usage, the term “desert” remains vague, its meaning varying with context. I once heard a story about a group of geographers from the Middle East being taken on a field trip to California’s Mojave Desert where they exclaimed, “Desert! What desert? There are shrubs and grasses everywhere. This is a lush steppe!”

In some contexts, areas with very little plant life can be called “deserts” regardless of how much precipitation they receive. The “volcanic deserts” of Iceland, Hawaii, and several other parts of the world fall into this category. Highly eroded landscapes underlain by soft sedimentary rocks often have bare slopes and can thus be called deserts even if they receive substantial amounts of rain. In the United States, however, the usual term for such landscapes is “badlands.” In Colombia, not surprisingly, they are called “desiertos” (deserts).
Colombia’s well-known Tatacoa Desert in Huila department is a classic example of badlands topography. As can be seen in the photo posted below, the eroded slopes are generally bare, but abundant vegetation can be seen in the background. Here one finds a tropical dry forest, or scrubland, with average annual precipitation or around 1,000 to 1,300 mm (39 to . 51 inches). Relatively high temperatures throughout the year combined with abundant sunshine contribute to the lack of vegetation in Tatacoa’s highly eroded areas.
The arid and semiarid belt of far northern South America, centered on Colombia’s Guajira Peninsula, is situated in a latitude belt and continental position that should, all other things being equal, receive much more precipitation than it does. It thus constitutes a “problem climate” as identified and analyzed by geographer Glenn Trewartha in his important 1961 book The Earth’s Problem Climates (University of Wisconsin Press). Trewartha accounted for this unusual climate by reference to: persistent northeast trade winds blowing along or across an east/west oriented coast, producing limited orographic lift over the relatively low, flat peninsula; coastal upwelling that cools sea-surface temperatures, stabilizing the lower atmosphere, reducing evaporation and suppressing convection; and the fact that the region lies to the north of the typical seasonal reach of the Intertropical Convergence Zone (ITCZ) for much of the year. Recent research, according to AI, also notes the “Caribbean Low-Level Jet (CLLJ), a persistent easterly wind maximum that enhances evaporation from land, transports moisture westward toward Central America (where it rains), and produces large-scale subsidence over the Guajira peninsula.”













































































