Tag Archives: Study in Argentina

Argentina is a presidential federal republic. According to the Constitution of 1853, amended several times, executive power is entrusted to the head of state, who is also head of the government and is elected by direct suffrage. With the 1994 amendment, the presidential term was reduced to 4 years and made renewable only once. Legislative power is entrusted to the National Congress formed by the Chamber of Deputies, whose members are elected by general suffrage, and by the Senate, whose members are chosen by the representative bodies of the various provinces. The Argentine judiciary is based on the European continental system, with influences of American derivation. In each province there is a Supreme Court and local courts; L’ main federal body is represented by the Supreme Court. The death penalty is no longer in force for ordinary crimes. The defense of the country is entrusted to the three traditional forces: army, navy and air force; military service is not compulsory and the minimum age for voluntary conscription is 18 years. Since 1884, education in the country is secular and free and compulsory schooling between the ages of 6 and 14. The fight in favor of literacy, waged during the government of Perón through five-year plans for the school (despite a rigid state control of cultural institutions) has helped to reduce to a large extent the illiteracy rate, which is among the lowest in the country. Latin America (2.3% in 2008). The education system is organized into primary education, which lasts 7 years and secondary education, which starts from 12 years of age and lasts 5 or 7 years. Higher education is given in numerous state and provincial universities (including Buenos Aires, 1821; Córdoba, 1613; La Plata, 1884; Rosario, 1968; Tucumán, 1914) and private universities. According to COUNTRYAAH, Argentina is a nation in South America, the capital city of which is Buenos Aires. The latest population of Argentina is 45,195,785. TRANSPORTHINT: Lists and descriptions of main religions and beliefs in Argentina, including religion demographics and statistics on Christianity, Islam, Judaism, etc.
CLIMATE
Being located in the thinnest portion of South America has a strong impact on the climate of Argentina, which therefore has the effects of continentality relatively attenuated: in fact, the most peculiar (and economically important) climatic area of ​​Argentina is the central one., pampeana, with a temperate climate, even if rainfall is scarce in certain areas; given, however, the considerable extension of the country in the sense of latitude (from 22º to 55º S), conditions vary significantly between the N and S, passing from a tropical or subtropical climate in Mesopotamia and Gran Chaco, with hot summers and mild winters (annual average 18-20 ºC), to a cold oceanic climate in Patagonia, where a record temperature of -33 ° C was recorded in 1907. The climate of the Andean region is naturally also affected by altitude and has typically mountainous characteristics (strong temperature variations, very harsh winters, etc.): in the Puna and in general in the Northern Andes, aridity is accentuated, so much so that, at the town of Rivadavia, a temperature of 48.9 ° C was recorded, the highest ever recorded in the subcontinent, while very abundant rainfall is recorded to the S where, due to the lowering of the Andean chain and the extreme thinning of the territory, the oceanic climate prevails everywhere. Southern Argentina is the only area subject to the action of the Pacific winds, given the barrier placed elsewhere by the Andes as they pass; on the opposite side the particular direction of the air masses promoted by the anticyclone of the South Atlantic means that it directly invests only the northernmost part of the country. Here, in fact, close to the Brazilian highlands, the most abundant precipitations occur, with maximums around 1800 mm per year; elsewhere it falls to the values ​​typical of semi-arid or even arid countries, with a general decrease proceeding from E to W: thus the Gran Chaco passes from over 1000 to 500 mm of precipitation, registering in the western area a typically tropical climate, characterized by winter from a long dry season. The Mesopotamian strip, on the other hand, has a subtropical monsoon climate without a dry season; in the Pampa it goes from 1000 mm of the coast (Pampa húmeda) to 600 mm of the interior (Pampa seca) where there is a steppe temperate climate, with very hot summers and mild winters. Patagonia is sub-desert, characterized by very severe winters, very high temperature ranges and rainfall between 200 and 400 mm per year; proceeding towards S, up to and including Tierra del Fuego, the rains increase due to the aforementioned oceanic influences, while temperatures drop significantly (annual average of 5 ºC): here the limit of perennial snow, which in the Northern Andes is 5000- 6000 m above sea level, descends to 1000 m above sea level on the Strait of Magellan. As far as the distribution of precipitation is concerned, there is a trend in the isoieties to assume a meridian trend, characteristic of South America and fundamentally due to the orientation of the Andean chain. The anomaly is even more marked if we consider the isotherms, especially those of January (ie the hottest month): that of 15 ºC develops from the extreme Patagonian coast to the pre-Andean area of ​​Tucumán. In the colder months a certain continentality removes the anomalous distribution of temperatures: an expression of this is the pampero, a cold and dry wind that blows from the SW into the Pampa (another frequent wind in the country is the norte, warm, which blows from the North). especially in summer). On the coasts, especially the Patagonian ones, the average values ​​are kept low by the cold current of the Falklands.