The Climates of South America

The continent of South America is a verysouthern most parts of Chile and Argentina. The
extensive continent in the North-South direction.summers are cool because these areas are
Its northern most part the Gulf of Venezuela is atlocated very far from the equator -at Punta
about 10 degrees north while the southern mostArenas in Chile located at 53 degrees South the
tip Cape Horn is almost at about 55 degreestemperature of the warmest month is only 52 F (
south of equator. As we know that chief factor11 C) and the coolest 35 F ( 3 C ). The range is
affecting the climate of a place is the latitude sotherefore only 17 F. This calls for an explanation.
we can expect a wide variation in the climate ofPlease note that as expected from a such a high
South America. Interestingly it is not so. Thelatitude the summer temperature would have
reason being that this continent has a conic shapebeen around 68 F which is typical of
and it becomes narrower and narrower as we gocool-temperate climate( London has 65 F ). The
towards the southern latitudes and due to thereason is that the southern most tip of the
combined influence of the Atlantic and the Pacificcontinent of South America is very narrow and
oceans, extreme variations in the temperaturesremains under the influence of both the Pacific
are not present.and the Atlantic oceans. Consequently the
The climate of South America can be divide intosummers are cool and winters mild. The rain is
the following seven climatic zones.light and is uniform throughout the year. The total
Tropical Climate:annual rainfall at Punta Arenas is 16 inches ( 400
This climate is found in the Central Brazil, Easternmm ) but even such a low rainfall is sufficient to
Peru and South Eastern Columbia. Thesustain vegetation since evaporation rate is
temperature remains high ( around 80 F or 27 C )retarded at such a low temperatures.
throughout the year. The rainfall is heavy; usuallyMediterranean Climate
greater than 80 inches ( 2000 mm) and is uniformCentral Chile exhibits the typical Mediterranean
all the year round and humidity is excessive.climate of dry warm summers and cool wet
There is no winter month. No month is below 70winters. The max temperature at Santiago, Chile
F (21 C ) and the range between the hottest andlocated in the heart of this region in the hottest
coolest month is very narrow. These areas liemonth of January is 67 F ( about 20 C ) and min
about 7 degrees south and north of the equator.in the month of July is 46 F ( 7 C ). The total
At Iquitos in Peru for example which is located atannual rain fall is 14 inches ( 350 mm ) of which
4 degrees south and 73 W, the total annual rainfallmore than 11 inches or 80 percent falls in the
is 103 inches ( 2600 mm) equally distributed in allwinter months from May to August. January is
months and no month receives less than 7 inchespractically dry. The temperatures in the hottest
(175 mm). To give you an idea of the heavinessmonth are less than the other Mediterranean
of rainfall compare it with London which has alocations in the Northern Hemisphere ( Rome 76 F
total annual rainfall of 23 inches ( 600 mm ). At) because Santiago is under the influence of cool
Iquitos the hottest month has a temperature ofpacific current in summer.
78 F ( 26 C ) and coolest of 74 ( 23 C ); a rangeDesert Climate
of only 4 F. Such a high temperature andAlmost all of the pacific coast of South America
abundant rainfall is responsible for one of thewhich contains a major part of Chile and south
thickest forests in the world which are foundwestern Argentina depicts this type of climate.
every where in this area. The weather for theThis is a very narrow strip which runs along the
foreigner is however trying for the high humidityAndes mountains and on the other side is the
combined with high temperature makes thepacific ocean. This is the reason that the stations
weather quite oppressive.located in this part of the world do not have that
Sub-Tropical Climateextremes of temperatures which are found in the
This type of weather is found in Northern andNorthern Hemisphere Deserts but the ares are
Southern Brazil, almost whole of Columbia, greaterone of the driest places on earth. Antofagasta at
part of Venezuela, Guyana, Surinam and French24 S and 70 W lies in the heart of the Atacama
Guiana. The rainfall is nether so heavy norDesert of South America which is known for its
uniformly distributed among all months.. There is adryness all over the world. Although the warmest
definite wet and dry season. The temperaturemonth is 72 F ( 22) and the coolest month is 61 F
range is also greater than that of the tropical( 16 C ) at Antofagasta which does not show any
regions. Rio de Janeiro in South Eastern Brazil isextremes of temperatures but the rainfall is
the best example of this type of Climate. Thepractically NIL in each month leading to a total
total annual rainfall for this station is 44 inchesannual rainfall which is negligible. Indeed there are
(1100 mm ) which is not meager but four monthssome areas in this region which have not received
from June to September each have less than 3rainfall for the last 400 years.
inches ( 75 mm ) of rainfall while March andMountain Climate
December record more than 5 inches ( 125 m ).A very long Mountain range runs across the
The coolest month is June with a temperature ofwestern edge of the continent between about 10
68 F ( 20 C ) and the hottest January with adegrees North Latitude and 50 degrees South
temperature of 78 F ( 26 C ) showing a range ofLatitude and is among the longest mountain
10. It may come to the reader as a surprise thatranges of the world. This is called the Andes. It
Jan. is hottest at Rio but remember that we arecontains many important cities of South America
in the southern hemisphere where the seasonslike Quito in Ecuador, Bogotá in Columbia
are reversed. The climate on the whole is lessand La Paz in Bolivia. All these cities are located
oppressive than that of the tropical one.2000 m ( about 7000 feet) above mean sea level.
Warm-Temperate ClimateAs we know that the temperature falls 1 degree
This type of climate is found in Argentina,F for every 300 feet or 1.6 C for every 1000
Uruguay and Paraguay. The characteristic featuresfeet so the altitude modifies the temperature of
are warm summers and mild winters. Rainfall isa place to a great extent. The typical example of
moderate and is uniform throughout the year.the effect of high altitude on temperature is that
The range between the hottest and coldestof Quito in Ecuador which lies directly on the
month is much greater than that of the twoEquator and being an Equitorial station one
regions described above. At Buenos Aires inexpects a constant hot and wet climate with
Argentina the total Annual Rainfall is 37 inches (unbearable humidity but due to its elevation of
about 900 mm ) equally distributed in all monthsabout 10,000 feet the climate is very pleasant.
so that no month is below 2.5 inch ( 50 mm). TheThe temperature remains in the range of 54-55 F
hottest month is Jan. with a temperature of 74 F( 12-13 C ) throughout the year and gives the
( 23 C ) and the coolest is July with 49 F ( 9 C );effect of an English Spring. That is why areas like
thus having a range of 35 F. There are nothese are called lands of perpetual spring. The rain
extremes of temperatures in this type of climatehowever is heavy and is equally distributed
and has been ideal for foreign settlement.. This isthrough out the year,
the reason that almost 90 percent of theThis concludes the account of climatic zones of
population of Argentina is of European origin.South America which is not a thorough account
Cool- Temperate Climatebut touches all the important features of different
These climatic conditions are found in theclimates found in this continent.