The Kalahari is not a "true" desert like the Sahara or Libyan Desert. It is a semi-arid savanna in Southern Africa, receiving enough rainfall (250–500 mm) to support grasses and scattered trees. Northern African deserts formed due to rain-shadow effects, subtropical high-pressure systems, and continental air masses that suppress precipitation. The Kalahari's climate is shaped by its position on the subtropical high-pressure belt and the influence of the Indian Ocean, resulting in a distinct ecological zone with seasonal rains and rich biodiversity, unlike the hyper-arid north.