Geography of Kenya
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The geography of Kenya is diverse. Kenya has a coastline on the Indian Ocean, which contains swamps of East African mangroves. Inland are broad plains and numerous hills. Central and Western Kenya is characterized by the Great Rift Valley home to three of Africa's highest mountains, Mount Kenya, Mount Elgon and Kilimanjaro. The Kakamega Forest in western Kenya is relic of an East African rainforest. Much larger is Mau Forest, the largest forest complex in East Africa.
- Total: 1 km2 (0.39 sq mi)
- Land: 569,140 km2 (219,750 sq mi)
- Water: 11,227 km2 (4,335 sq mi)
- Total: 3,477 km (2,161 mi)
- Border countries: Ethiopia 861 km (535 mi), Somalia 682 km (424 mi), Sudan 232 km (144 mi), Tanzania 769 km (478 mi), Uganda 933 km (580 mi)
- 536 km along the Indian Ocean.
- Continental shelf: 200 m depth or to the depth of exploitation
- Exclusive economic zone: 200 nmi (370.4 km; 230.2 mi)
- Territorial sea: 12 nmi (22.2 km; 13.8 mi)
The climate of Kenya varies by location within Kenya: from mostly cool every day, to always warm/hot. The climate along the coast is tropical. This means rainfall and temperatures are higher throughout the year. At the coastal city Mombasa, the air heats from cool to hot, almost every day (see chart below). The further inside Kenya, the more arid the climate becomes. An arid climate is nearly devoid of rainfall, and temperature swings widely according to the general time of the day/night. For many areas of Kenya, the daytime temperature rises about 12 °C (53.6 °F), almost every day.
Elevation is the major factor in temperature levels, with the higher areas, on average, as 11°C (20°F) cooler, day or night. The many mile-high cities have temperature swings from roughly 50–79 °F (10–26.1 °C). Nairobi, at 1,798 m (5,899 ft) or 1.798 km (1.12 mi), ranges from 49–80 °F (9.4–26.7 °C), and Kitale, at 1,825 m (5,988 ft) or 1.825 km (1.13 mi), ranges from 51–82 °F (10.6–27.8 °C). The overnight lows are not like the " Garden of Eden" because, at night, heavy clothes or blankets are needed, in the highlands, when the temperature drops to about 50–54 °F (10–12.2 °C) every night.
At lower altitudes, the increased temperature is like day and night, literally: like starting the morning at the highland daytime high, and then adding the heat of the day, again. Hence, the overnight low temperatures near sealevel are nearly the same as the high temperatures of the elevated Kenyan highlands. However, locations along the Indian Ocean have more moderate temperatures, as a few degrees cooler in the daytime, such as at Mombasa (see chart below).
There are slight seasonal variations in temperature, of 4 °C or 7.2 °F, cooler in the winter months. Although Kenya is centered at the equator, it shares the seasons of the southern hemisphere: with the warmest summer months in February-March and the coolest winter months in July-August, although only a few degrees cooler.
|Climate Data for Mombasa (at Indian Ocean)|
High value F
Low value F
High value C
Low value C
Kenya’s terrain is composed of low plains that rise into central highlands that are, in turn, bisected by the Great Rift Valley.
8.01% of the land is arable. Permanent crops occupy 0.97% of the land. Other uses make up the rest of Kenya's land. (2005)
1030 km² of Kenya' land is irrigated.(2010)
Natural hazards include recurring drought and flooding during the rainy seasons.
Current issues that threaten the environment at the moment include water pollution from urban and industrial wastes; degradation of water quality from the increased use of pesticides and fertilizers; deforestation; soil erosion; desertification and poaching.
- Party to: Biodiversity, Climate Change, Desertification, Endangered Species, Law of the Sea, Marine Dumping, Marine Life Conservation, Nuclear Test Ban, Ozone Layer Protection, Ship Pollution ( MARPOL 73/78), Wetlands, Whaling
- Signed, but not ratified: none of the selected agreements
- The Kenyan Highlands comprise one of the most successful agricultural production regions in Africa.
- There are glaciers on Mt. Kenya.
- Unique physiography supports abundant and varied wildlife of scientific and economic value.