El
Sur del Sur
The Southernmost South Our
Land CLIMATEDue
to its vast territory, Argentina presents a remarkable climatic diversity.
In this sense, various geographic factors have a direct bearing, determining
the climatic characteristics of the different regions. One
of these factors is latitude: the Argentine Republic is characterized
by its great latitudinal development: from 21º 46' to 55º
58' S. This is basically the origin of the climatic variation in
the country.
Otherwise, the mountain
ranges extending from north to south in the Argentine west are a relief factor
facilitating the circulation of air masses in the east of the country and determining
different kinds of winds. Furthermore,
relief influences temperatures insofar as the higher the altitude, the lower
the temperature. The
presence of the sea, which, in the case of the Argentine territory,
constitutes a natural boundary to the east, exercises a moderating action, diminishing
the thermal range.
Different meteorological
factors act on the Argentine territory, some of them are local, whereas
the others originate beyond the Argentine boundaries, such is the case of the
warm and humid winds coming from the Atlantic anticyclone and affecting
the regions located to the north of Patagonia or the west winds coming
from the Pacific anticyclone, as well as the cold winds from the Antarctic
anticyclone. These three winds affect the Argentine climate in a permanent
way, unlike the local winds, which include:
The
Zonda, which is warm and dry, generally blowing between May and October
and originating to the east of the pre-cordillera in La Rioja, San Juan and
Mendoza; The Sudestada,which originates in the Pampa
littoral and is characterized by its high humidity content; The Pampero, coming from the south-west, is
cold and dry, and blows mainly in summer, after several days of constant increase
of temperature and humidity; Tornadoes, Tornadoes, which consist in an
air mass in the form of a vertical funnel reaching a rotating movement of about
310 mph (500 kmph), originate between October and March in the Plata Basin.
Besides, there
are also frequent snowfalls in the Andean area, as well as
frosts (if only coincidentally with the advance of cold winds from the
South Pacific or in high mountain areas and the Patagonian plateaus) and hail,
which can fall in the whole territory, especially between September and December.
KINDS
OF CLIMATE Warm: It
is found in the north-eastern angle of Argentina. Due to the decrease of the
oceanic influence towards the west and to the modifications of the mountainous
relief, there are three varieties of this kind of climate: sub-tropical
without dry season, sub-tropical with dry season and sub-tropical
of the sierras.
Mild: The
amount and distribution of rainfalls determine two varieties of mild climate:
to the east, the "Pampeano" (of Pampa) or humid and to the west,
there is a transition band towards arid climate. The average temperature
is 59º F (15º C).
Cold: There
are two kinds: the humid or oceanic cold, with an average temperature
of around 45º F (7º C), and the nival cold prevailing in
Antarctica.
Arid:
According
to the altitude and latitude, this climate shows four varieties: "high-mountain"
arid, with a temperature depending on altitude and a very wide thermal range;
"sierras-and-fields""arid with an average temperature of about 18º
C; the "steppe" arid, with an average temperature of around 18º
F (15º C) and presenting frequent frosts, which occur even in summer; and
cold arid, with an average temperature of about 50º F (10º
C), a fairly wide thermal range and frosts occurring the whole year.
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