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
Fog desert ranges allow for maritime winds to settle in specific geographic areas, which is a common theme in fog deserts. The Andes Mountain range is the land form that divides Chile and Peru into inland and coastal regions and allows for the fog desert to form along the Pacific coast. In the Atacama Desert, plant coverage can be as high as 50% in the center fog zone to as low as no life whatsoever above the fog line. Within arid fog deserts with low precipitation levels, fog drip provides the moisture needed for agricultural development. The diverse sections within a fog