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WORLD CLIMATES
The different climates of the world
run in broad zones around Earth
on either side of the equator. They
range from hot and rainy climates
at the equator to cold climates at the
poles. There are five main climatic
zones, each of which is shown on
this map by a different color.
SOME PARTS OF THE WORLD, such as the tropical rain forests of South
America, are hot and damp throughout the year. Other regions, such as the
Arctic, have long, freezing winters. Conditions such as these are known as
the climate of an area. Climate is not the same as weather. Weather can
change within minutes; climate describes a region’s weather conditions
over a long period of time. Every region has its own climate. This depends
on how near it is to the equator, which governs how much heat it gets from
the sun. Landscape also influences climate; high mountain regions, such as
the Himalayas, are cooler than nearby low-lying places. The ocean can
prevent a coastal region from getting very hot or very cold, while the weather
in the center of a continent is more extreme. The climate of a region affects
landscape and life—clothing, crops, and housing. But climate can change.
Today climatologists, people
who study climates,
believe that the
world’s climate
is gradually
warming up.
SUN AND CLIMATE
The sun’s rays warm the equator
directly from above, making the
tropics hot. Away from the
equator, the sun’s rays are less
direct, making climates cooler.
SAHARA DESERT
The Tuareg nomads are one
of the few peoples that live
in the punishing climate of
the Sahara Desert, coping
with the searing heat of the
day and the freezing
temperatures at night.
TEMPERATE CLIMATE
Warm summers and cool
winters feature in warm
temperate climates. Rain may
fall all year, or the summer
can be dry and sunny, as in
Mediterranean regions.
Away from the
equator, the sun’s
rays are spread
over a wide area.
In temperate
climates, trees
shed their leaves
in the winter.
COOL FOREST CLIMATE
Summers are cool and short,
and winters are long and cold.
Pines and other conifers grow
in huge forests that cover much
of the land.
TROPICAL CLIMATE
It is hot all year round in tropical
regions, and torrents of rain
usually fall every afternoon. Rain
forest covers much of the land. In
regions where wet and dry seasons
occur, tropical grasslands grow.
DESERT CLIMATE
In the dry, barren deserts,
cold, clear nights usually
follow burning-hot days.
However, high mountain
deserts may have cold,
dry winters.
THE FREEZING ANTARCTIC
Only hardy creatures, such as
penguins, can survive amid the
ice and snow of the Antarctic.
POLAR CLIMATE
It is cold all year, and ice and
snow always cover the ground.
No crops grow, and the few
people who live there hunt
animals for food.
The Sahara
is the largest
desert in the
world.
Climates
CLIMATIC CHANGES
Great climatic changes,
such as ice ages, come and
go during thousands of
years. But severe changes
in climate can also occur
suddenly or within a few
years. Dust from volcanic
eruptions can obscure the
sun, making a climate
cooler. Changes in winds
can cause rainfall to shift
from a region, bringing
drought. Human activities,
such as pollution, also
affect climate greatly.
GREENHOUSE EFFECT
The atmosphere works like
a greenhouse, trapping the
sun’s heat and warming Earth.
Pollution in the air traps more
heat, making Earth warmer.
Unless pollution is reduced,
Earth’s climate could be changed
Escaping heat
Trapped
heat
Sun’s
rays
The treeless
landscape of
the polar regions
is called
the tundra.
Find out more
Atmosphere
Earth
Glaciers and ice caps
Weather
Wind
The cool forest climate
exists only in the northern
half of the world.