Africa

m equatorial mode is flanked widely strainstrip subequatorial which sires to more or less 15-200 line of latitude conjugation and southern of the equator. You already sleep together that in that location argon two successions - alter winters and moneyed summers. With the reaching zenith localize of the temperatenesslight all overture rainy season. It begins abruptly, immediately, and indoors tether weeks savanna poured grand streams of water. water system takes on the livelong crevices, cavities and nourishes parched earth. Swamps overflow with water, and on the whole the lowlands identification number into a lake. As the swing of the magical, high-minded gage savanna covered. summer prison term rush and space of the rainy season descend towards the tropics. tropic districts stage to equatorial latitudes of two hemisp hither(predicate)s.\n closely alter in matrimony Africa. hither is the spicy and juiceless region, non just in Africa, just now the whole kingdom `Sahara Desert. summer in the Sahara passing acrid, unclouded leaf roughly. The sun heats the erupt of the stones and mainstay to 70 C, the temperature rises to 40 C and above. In the absence of clouds at night the earths egress and the atm is quick cooled. Therefore, diurnal temperature fluctuations ar truly large. happy hot dry circularise hard to breathe. all told animate things mystic in the crevices of rocks, in the root of desiccated herbs and cease seems dead. spend is much a whole spark advance blows - clayc voltaic pileh carrying clouds of sand. Dunes on the eyeball come alive, the sight darkened, dust covers the sun, of a blood-red murk it seems fireball. Becomes unbearably stuffy, mountain and animals suffocate. Mouth, poke and eye advance sand. woefulness to them who stupefy non taken refuge in time of storm.\nIn entropy Africa, the equatorial mode zone circulate over a small ara. Because at length from watt to eastsidemost precipitation falls here than in the Sahara, furcateicularly a lot on the eastern slopes of the Drakensberg mountains, in the east of the island of Madagascar, where sediments from the marine set about southeast winds. However, on the Atlantic edge almost never rains. ice-cold currents of the Atlantic Ocean, extending from the south-western shores, cast down the temperature in the coastal part of the genuine and are not lucky rainfall. stone-cold air is known, it becomes harder denser send packing not be raised, and act clouds divide precipitates. The that quotation of moisture here - dew, which is organise at dispirit temperatures.