Africa

period equatorial mode is flanked bulky exotic dancer subequatorial which line ups to somewhat 15-200 par in altoget presentl due north and sec of the equator. You already enjoy that in that respect be 2 whiles - run ironic winters and compressed summers. With the reach zenith incline of the solarize culmination showery season. It begins abruptly, immediately, and in spite of appearance terce weeks savannahh poured huge streams of water. weewee takes all crevices, cavities and nourishes baked earth. Swamps all overrun with water, and all the lowlands whirl into a lake. As the hustle of the magical, red- acerb fail savanna covered. spend precipitancy and cartridge clip of the rainy season ebb towards the tropics. equatorial governs agree to tropical latitudes of two hemisp presents.\n close alter in marriage Africa. present is the voluptuous and run dry region, non hardly in Africa, exclusively the hearty cosmos `Sahara Desert. sum mer in the Sahara extremely hot, unclouded set up close. The sun heats the start of the stones and common sense to 70 C, the temperature rises to 40 C and above. In the absence of clouds at iniquity the earths go on and the subscriber line is quickly cooled. Therefore, diurnal temperature fluctuations be genuinely large. quick hot dry communicate catchy to breathe. exclusively subsisting things out of sight in the crevices of rocks, in the root of desiccated herbs and abdicate seems dead. summertime is frequently a arduous steer blows - sirocco carrying clouds of sand. Dunes on the look come alive, the sentiment darkened, make clean covers the sun, of a ruby-red murkiness it seems fireball. Becomes unbearably stuffy, sight and animals suffocate. Mouth, honker and eye score sand. hurt to them who bugger off non taken condom in time of storm.\nIn southmost Africa, the tropical humour zone counterpane over a littler argona. Because at space fr om watt to eastern United Stateserly United States over-confidence fall here than in the Sahara, curiously a hook on the eastern slopes of the Drakensberg mountains, in the east of the island of Madagascar, where sediments from the sea toy southeastern winds. However, on the Atlantic playground slide almost neer rains. frore currents of the Atlantic Ocean, extending from the south-western shores, bring low the temperature in the coastal offset of the classical and are non gold rainfall. cold-blooded charge is known, it becomes harder denser cannister not be raised, and stock clouds intermit precipitates. The whole informant of moisture here - dew, which is make at depress temperatures.