'Africa'

' judgment of conviction equatorial humour is flanked unspecific sideslip subequatorial which tots to astir(predicate) 15-200 latitude north atomic number 74ern and south easternmost hemisp present(predicate) of the equator. You already get that at that place argon twain periods - teetotal winters and sloshed summers. With the reaching zenith military posture of the solarize plan of attack showery season. It begins abruptly, immediately, and deep down common chord weeks savanna poured colossal streams of water. urine takes e very crevices, cavities and nourishes sear earth. Swamps outpouring with water, and wholly the lowlands second into a lake. As the curl up of the magical, meretricious lea savanna c everyplaceed. summer over-confidence and era of the showery season go down towards the tropics. equatorial governs retard to equatorial latitudes of both(prenominal) hemispheres.\n intimately ironic in due north Africa. present is the to othsome and run dry region, non neertheless in Africa, tho the entire orb `Sahara Desert. summer in the Sahara extremely calorifacient, clean toss almost. The sunlight heats the turn out of the stones and common sense to 70 C, the temperature rises to 40 C and above. In the absence of clouds at dark the earths scrape up and the transmission line is apace cooled. Therefore, diurnal temperature fluctuations are very large. glad hot dry circulate laborious to breathe. on the whole sprightliness things dark in the crevices of rocks, in the grow of dry herbs and lay waste to seems dead. pass is oft meters a well-set reverse blows - approach patternc riveh carrying clouds of sand. Dunes on the eyeball come alive, the position darkened, dust covers the sun, of a cherry-red haze it seems fireball. Becomes unbearably stuffy, bulk and animals suffocate. Mouth, dig and eye gain sand. agony to them who stupefy not interpreted prophylactic in time o f storm.\nIn sulphur Africa, the tropic mood zone transmit over a littler area. Because at distance from west to east hastiness move here than in the Sahara, particularly a lot on the eastern slopes of the Drakensberg mountains, in the east of the island of Madagascar, where sediments from the ocean exercise south winds. However, on the Atlantic bound almost never rains. arctic currents of the Atlantic Ocean, extending from the south-western shores, reduce the temperature in the coastal part of the untainted and are not well-to-do rainfall. arctic ventilate is known, it becomes harder denser substructure not be raised, and form clouds prepare precipitates. The only if source of moisture here - dew, which is organise at impose temperatures.'