Geography of South Africa ore from the interior. South Africa is largely a dry country, with most of its western regions being semi-desert. The rainfall increases in the east, (the Highveld, KwaZulu-Natal, and the Eastern Midlands), and falls primarily in summer. The narrow southern coastal strip receives all-year rainfall in the east (the Garden Route), and winter rainfall in the west (on the Cape Peninsula and its surrounds). The summers are warm to hot, while the winter temperatures can vary, depending on locality from bitterly cold to cool. Thus the Karoo, which occupies a large part of the western Central Plateau, has a climate
Ryn Desert can drop to a low of . Many small towns are scattered throughout the Ryn Desert, and population density is between 1 and 15 people per square mile. The Ryn lies in a semi-arid climate zone, and receives very little rainfall. High winds sweep across the desert, and in 2001 a dust storm in the Baltic Sea was determined as originating in the Ryn Desert. A study of long-range dust transportation to the Baltic Sea region—by analyzing dust pollution in Scandinavia, showed that aerosol concentrations there were influenced more by the Ryn Desert region than the Sahara Desert in Africa.