Tag Archives: Study in Ethiopia

The surface of Ethiopia occupies a large part of the highlands between Eritrea and the Nilotic depression. The territorial changes that gave Ethiopia the configuration, which included Eritrea, a country that after a long liberation struggle achieved independence in 1993, are due to the colonial era. The borders with Somalia are theirs. vault arbitrary: in the border areas the guerrilla of the Ogadèn secessionists is active. However, the current territory of Ethiopia substantially corresponds to that of the kingdoms formed since the first centuries AD. C. and remained independent, even at the cost of some territorial concessions (except for the brief period of Italian colonial domination from 1935 to 1941). This is an almost unique case in Africa, where present-day states have mostly arisen as a result of Arab expansionism and artificial colonial subdivisions. Ethiopia is in fact the only African country that has managed to resist colonization, has played an important role in the region and has developed its own political and cultural tradition. Ethiopia has managed to preserve its identity thanks to two factors: Coptic Monophysite Christianity, which is the binding factor for the various peoples inhabiting the plateau; the natural conditions of the territory, similar to a single large defensive bastion. At the beginning of the century. XXI, however, the country presents a contradictory image: the events of recent decades have brought to the fore a state that appears very poor and does not seem able to satisfy the basic needs of its residents, but at the same time spends much more than enough to feed the population and pursues a regional power policy. According to COUNTRYAAH, Ethiopia is a nation in Eastern Africa, the capital city of which is Addis Ababa. The latest population of Ethiopia is 114,963,599. REMZFAMILY: Lists and descriptions of main religions and beliefs in Ethiopia, including religion demographics and statistics on Christianity, Islam, Judaism, etc.
CLIMATE
Due to its geographical position, Ethiopia has a climate that can be defined as tropical with two seasons, one of which is dry in winter (October-March) and rainy in summer (April-September). But if the latitudinal factor actually determines an average decrease in precipitation from the equator towards the tropics, the altitude and the arrangement of the relief profoundly influence not only the rains but also the temperatures and winds. It is also necessary to consider the proximity of the Asian continent, separated only by the narrow Red Sea. So, in January, to ‘ anticyclone West Asia is directly opposed the cyclone of central Africa. The resulting winds, blowing from NE to SW, rather cold and dry, collect little humidity on the Red Sea, discharging it immediately on the coasts and on the Eritrean escarpment. In July the situation is reversed and the equatorial winds, hot and humid, which hit Ethiopia coming from both the SE and SW discharge their waters on the plateaus. This corresponds to a marked distributional difference in precipitation passing from the highland to the coastal plain of Eritrea and to Danakil: in the latter there is a clearly arid regime (up to 50 mm per year), in the plateau it generally exceeds 1000 mm per year, with higher values ​​ (up to 1800 mm) on the central reliefs and in the western areas, and decreasing values ​​towards the E and SE, as well as towards N (Eritrea). A particular regime has the slope exposed to the Red Sea, where there is winter and summer rainfall with totals that in some areas exceed 1000 mm per year. As far as temperatures are concerned, altitude plays a decisive role; it is therefore necessary to distinguish between the highland areas and the plains, with average differences of the order of 8-14 ° C. Generally in the regions located around 2000 m the annual average is around 16-18 ° C, with a very low annual temperature range of 4-5 ° C and even less: Addis Abeba, located at 2370 m of altitude, has an average annual temperature of 16 ° C, with an average of 15.9 ° C in January and 14.9 ° C in July. The daily temperature change is more pronounced: in winter, during the night, the thermometer can even drop below freezing. The plains, on the other hand, are among the hottest areas on Earth, reaching even 50 ° C in some places. The hikes, both annual and between the absolute maximums and minimums, are significant: in Massawa the average temperature ranges from 25.5 ° C in January to 34.5 ° C in July, while the absolute maximum is 47.5 ° C and the absolute minimum of 14 ° C. Local topographical elements are due to the fact that in some areas the hottest months are winter and the coldest are the summer months: this is the case, for example, of Addis Abeba and Gambela (27.2 ° C on average in January, 25, 6 ° C in July), located in southwestern Ethiopia (region of Ilubabor).