Kenya’s temperatures vary dramatically, with the highlands experiencing considerably cooler temperatures than the coastal and lowland regions. Kenya’s average annual precipitation is typically 680 mm, ranging from less than 250 mm in the northern ASALs areas to about 2,000 mm in the western region.
How Is Kenya’s Climate?
Seasonal climatic changes are controlled by the large-scale pressure systems of the western Indian Ocean and adjacent landmasses. From December to March, northeast winds predominate north of the Equator, while south-to-southeast winds dominate the south of it. These months are fairly dry, although rain may occur locally. The rainy season extends from late March to May, with air flowing from the east in both hemispheres. From June to August there is little precipitation, and southwest winds prevail north of the Equator as southeast winds prevail in the south.
In the Lake Victoria basin, annual precipitation varies from 40 inches (1,000 mm) around the lakeshore to more than 70 inches (1,800 mm) in the higher elevations in the eastern areas. The lakeshore has excellent agricultural potential because it can expect 20 to 35 inches (500 to 900 mm) in most years. Daily maximum temperatures range from 80 °F (27 °C) in July to 90 °F (32 °C) in October and February.
In the Rift Valley, average temperatures decrease from about 84 °F (29 °C) in the north to just over 61 °F (16 °C) around Lakes Nakuru and Naivasha in the south. The adjacent highlands are generally moderate, with average temperatures ranging between 56 and 65 °F (13 and 18 °C). The floor of the Rift Valley is generally dry, while the highland areas receive more than 30 inches (760 mm) of rain per year. The reliable precipitation and fertile soils of the Mau Escarpment form the basis for a thriving agricultural sector.