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Rainfall is the key determinant of climatic differentiation, and it decreases rapidly from north to south and in proximity to the coast.
The Maiombe forest in the northern part of the Cabinda exclave receives the greatest amount of rainfall, about 70 inches (1,800 mm) per year, and Huambo, on the Bié Plateau, receives 57 inches (1,450 mm).
The central part of the plateau is drained by the Cuanza (Kwanza), the largest river entirely within Angola’s frontiers, which is about 620 miles (1,000 km) in length.
The average annual temperature in Soyo, for example, at the mouth of the Congo, is 79 °F (26 °C), whereas in Huambo, on the Bié Plateau, it is 67 °F (19 °C).
Until the late 19th century, parts of Angola were covered with dense rainforest, mainly in the northern part of the Cabinda exclave, the western edge of the Malanje highlands, the northwestern corner of the Bié Plateau, and along some rivers in the northeast.
Droughts frequently afflict the country, especially in the south.
Temperatures vary much less than rainfall, however, and generally decrease with distance from the Equator, proximity to the coast, and increasing elevation.
Angola is roughly square in shape, with a maximum width of about 800 miles (1,300 km), including the Cabinda exclave, which is located along the Atlantic coast just north of Angola’s border with the Democratic Republic of the Congo.