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
Climatic regions of India The region towards the North, East and South of the Tropical Desert zone running from Southern Punjab, Haryana and, Western Uttar Pradesh to Gird and Malwa regions in Western Madhya Pradesh and eastern fringes of Rajasthan and from there onwards to the Central Gujarat and Kathiawar regions of Gujarat state experience this climate type. India's capital city Delhi lies in this climatic zone. This climate is a transitional climate falling between tropical desert and humid sub-tropical zone, with temperatures which are less extreme than the desert climate. The annual rainfall is between 30 and 65 cm but is very unreliable