Haboob Guinea. Haboobs in Australia may be frequently associated with cold fronts. The deserts of Central Australia, especially near Alice Springs, are particularly prone to haboobs, with sand and debris reaching several kilometers into the sky and leaving up to of sand in the haboob's path. As with haboobs in the Middle East, haboob occurrences in North America are often created by the collapse of a thunderstorm. This is a local or mesoscale event, and at times of extreme drought they can originate in agricultural regions. Some of the most famous dust storms of the Dust Bowl and similar conditions later
Sechura Desert from the Andes support intensive irrigation-based agriculture. Within Peru, the desert is described as the strip along the northern Pacific coast of Peru in the southern Piura and western Lambayeque regions, and extending from the coast 20–100 km inland to the secondary ridges of the Andes Mountains. At its northern end near the city of Piura, the Sechura Desert transitions to the Tumbes-Piura dry forests ecoregion. Comprising much of eastern Lambayeque Region, this habitat is composed of equatorial dry forests. The total area of the Sechura Desert is 188,735 km². While a desert, the Sechura has been subject to flooding