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Published byBarnaby Parrish Modified over 8 years ago
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The African farmer is affected by climate, vegetation and soils
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Climate Similar climatic patterns north and south of equator Equatorial, tropical wet and dry, desert, and Mediterranean climates Differ in terms temperature, rainfall, and evaporation.
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Temperatures high throughout Mean annual temp. ranges from 15 to 33 C (59 to 91 F) Highest temp. not at the equator –Continuous cloud cover and moisture protect against the sun's rays.
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Temperatures Fairly constant at equator Fluctuates farther north or south of equator daily and annually Mali--averages 30 deg. C Congo (Zaire) averages 25 deg. C
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Difference between means for the coolest and warmest months Big difference Algeria Small difference Congo
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Day-time highs and night-time lows Algeria: large variation Congo: small variation
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Rainfall distribution More critical than temperature ranges Explained by the Inter- tropical Convergence Zone
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Inter-tropical Convergence Zone (I.T.C.Z.) Low pressure zone near equator Trade winds converge, accumulate, air ascends causes rain
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I.T.C.Z. Not stationary Oscillates between 20 degrees north and 25 degrees south. Irregular and unpredictable
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Direct correlation between the I.T.C.Z. and rainfall patterns. January-- I.T.C.Z. rainfall at Equator and south
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July-- I.T.C.Z. shifts; rainfall is north of equator.
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Only equatorial zone receives rain throughout the year Both rainbelts overlap About 8% of Africa, the Congo (Zaire) Basin and the coast of West Africa, receive >1600 mm of rain annually
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50% of the continent is arid or semi-arid Agriculture is constrained by water availability in over half of Africa
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Africa has a negative water balance Evaporation> rainfall, leads to water deficits –Evaporation is high because of high temp. and radiation. Only Equatorial Africa has water surplus
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I.T.C.Z. is important for the African farmer I.T.C.Z. causes distinct dry season except in equatorial areas
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Length of the dry season – 3 - 8 months just North and South of Equator – up to 8 - 10 months further away
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Farming and food production determined by Length of the dry relative to the wet season
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Lengthy Dry Seasons Proper storage systems become part of the food production cycle
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Rains a crucial period for the farmer Farming in a restricted rainy season Planting and weeding in a short period of time High labor demands
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Local traditional varieties Are adapted to –Rainfall conditions –Plant diseases and pests
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Local traditional varieties Evolved over thousands of years Some were domesticated in the area
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Crops domesticated in West Africa millet sorghum okra watermelon fluted pumpkin kola (coca cola ) cotton sesame
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Crops domesticated in Ethiopia Coffee Teff Enset Cress Castor (castor oil)
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Rainfall variability is high The smaller total amount, the higher the variability
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Other factors in climate Warm or cold ocean currents High plateau of East Africa The Great Escarpments Cold fronts from Antarctica Thunderstorms in equatorial Africa
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Regional distortions The Mediterranean climate –Northern and Southern Africa The Sahara desert –Brought about by dry air masses coming from Arabia
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VEGETATION Correlates strongly with rainfall patterns Dry conditions -- desert-like vegetation Semi-arid conditions--steppe
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VEGETATION Sub-humid conditions--savannas Wet conditions-- forests and rainforests
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Vegetation Continuum rainforest-forest--savanna--steppe--desert No true boundaries exist
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From the equator to the desert Fewer and smaller trees Increased grassland-like vegetation Decreased diversity of species
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Vegetation zones resemble north and south of equator Rainforests cover only 8- 10% Africa-- continent of savannas and deserts
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Rainforests Poor soils Nutrients recycled
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Destruction of rainforests Rapid Large amounts cleared yearly
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Savannas Between forests, steppes, and deserts
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Nearer to the equator Trees dominate grasses Woodland savanna
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Further north or south of the equator-- a distinct dry season Savanna grasslands Woodland savanna
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Characteristics of savanna Herbivores (rhinoceros, elephants and giraffes) predators (lions)
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Characteristics of savanna areas Baobab trees (girths of 30 feet +) Huge bodies of granite
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Steppe Transition zone between savannas and deserts Narrow bands on either side of the savanna.
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Semi-arid conditions e.g., Kalahari Desert Sparse vegetation Plants-- extremely scrubby Thorn trees
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Under extreme conditions Cactus and aloe, growing in almost bare soils. Vegetation- a function of climate and soils.
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Steppes: extensive livestock grazing Drier areas used by pastoralists
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Agriculturalists occupy wetter areas Competition between the two groups for best land
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Rainfall variability and drought High in the between savannas and deserts Above-average alternates with low rainfall Produces droughts
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1970s: Sahel area (West Africa) 1980s: Ethiopia 1990s Southern Africa, Horn of Africa 2002-3 Southern Africa Massive crop failures Famine and starvation (people and livestock)
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1/3 of Africa taken up by three main deserts Sahara, 1/4 of the land mass of the continent Namib Kalahari, a semi-arid region rather than true desert
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Desert proper Areas receiving less than 250 mm of rain per year Little vegetation Daily temp. fluctuate > 35 C (95 F) Seasonal av. temp. > 40 C (104 F)
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