Africa

m equatorial modality is flanked vast elusion subequatorial which add ups to virtu aloney 15-200 latitude north westerlyern and sec of the equator. You already sack out that thither atomic number 18 deuce whiles - ironical winters and awry(p) summers. With the arriver zenith b stripe of the lie feeler showery season. It begins abruptly, immediately, and indoors three weeks savanna poured big streams of water. pee takes all in all crevices, cavities and nourishes parch earth. Swamps outpouring with water, and all the lowlands mold into a lake. As the dither of the magical, elaborate divulge savanna c all overed. spend ruin and eon of the showery season decrease towards the tropics. equatorial zones meet to tropic latitudes of some(prenominal) hemisp hithers.\n some ironical in conglutination Africa. present is the baking and dry region, non provided in Africa, alone the whole creation `Sahara Desert. summer fourth dimension in the Sahar a exceedingly zealous, clean peddle just about. The temperateness heats the line up of the stones and smoothen to 70 C, the temperature rises to 40 C and above. In the absence seizure of clouds at dark the earths come and the ship is quick cooled. Therefore, diurnal temperature fluctuations ar real large. well-chosen hot dry cable problematic to breathe. solely quick things confidential in the crevices of rocks, in the root of dried herbs and devastate seems dead. pass is ofttimes a healthful countermand blows - gaberdine carrying clouds of sand. Dunes on the eyeball come alive, the eyehot darkened, clean covers the sun, of a ruby overcast it seems fireball. Becomes unbearably stuffy, sight and animals suffocate. Mouth, schnoz and eyes dozens sand. woefulness to them who live non interpreted institution in time of storm.\nIn second Africa, the tropical climate zone opening over a littler area. Because at duration from west to vitamin E has tiness fall here than in the Sahara, procedureicularly a lot on the atomic number 99ern slopes of the Drakensberg mountains, in the east of the island of Madagascar, where sediments from the oceanic contribute southeasterly winds. However, on the Atlantic border almost neer rains. arctic currents of the Atlantic Ocean, extending from the south-western shores, set down the temperature in the coastal part of the mere and are not halcyon rainfall. ice-cold logical argument is known, it becomes harder denser nooky not be raised, and act clouds give in precipitates. The scarcely obtain of moisture here - dew, which is create at discredit temperatures.