Past
climate change
The Earth’s climate
has always been changing. Only 20,000 years ago, much of Northern Europe was
still covered in an enormous glacier that was up to three kilometers thick! The
Alps and the Pyrenees mountains were covered with smaller ice caps. Sudden climate
shifts happened quite frequently during the Ice Age, and made the ice expand or
contract. In the cold climate south of the ice-covered areas, small groups of
people hunted reindeer, wild horses, and bison.
People living in the
Ice Age left behind stone tools and fantastic cave paintings. But their way of
life was about to disappear. Over thousands of years, the Earth’s orbit around
the sun changed so that the summers became warmer, and the ice began to melt.
The Ice Age ended around 10,000 years ago. Since then, the climate in Northern
Hemisphere has been warmer and far more stable. Over the last 10,000 years of
milder climate, people developed agriculture, cities, and civilization – which
would have been far more difficult during the Ice Age.
We will always be at
risk of unexpected and unpleasant climate changes from natural causes. For
example, around 400 years ago Europe experienced a relatively cold period
called the Little Ice Age (it was not as cold as a real ice age). What is
different about the situation today is that we risk rapid changes in climate
caused by people. Because of our increasing emissions of CO2 and other
greenhouse gases, we expect that over the next hundred years we will see that
fastest warming of the Earth since the end of the Ice Age.
From
local to global problems
As long as we humans
have existed on Earth, we have affected the environment around us. But in the
past, the effects of our hunting or agricultural activities were
basicallylocal. This changed with the Industrial Revolution that began round
1750 and accelerated in the 1800s and 1900s. A revolution is a dramatic social
change.
The
Industrial Revolution took place when people began to mass produce goods in
large factories using machines that ran on energy from coal, and later, oil,
natural gas, and electricity. This made it much easier for people to produce
goods, and helped the development of modern technology. In pre-industrial times
– that is, the time before the Industrial Revolution – there were no trains,
cars, planes, electric lights, factories, telephones, or televisions.
The more we produce
and consume, the more we affect the environment around us. During the last 50
years, for the first time in history we have seen clear signs that human
influence affects the environment of the entire planet; we are creating
environmental problems that are not only local but also global. One of these
global environmental problems is the risk of man-made climate change, also
known as global warming.
Global
climate change
Man-made climate
change occurs because we emit greenhouse gases to the atmosphere. These
emissions come from many sources, including the factories and agriculture that
supply us with food and other material goods, power plants that provide us with
electricity, and cars and planes that take us where we need to go.
Greenhouse gases
affect the Earth’s climate by increasing thegreenhouse effect, which is a
natural phenomenon whereby water vapor, CO2, and other gases in the atmosphere
allow sunlight to pass through, but then absorb much of the heat from the earth
that otherwise would have escaped to outer space. Without the natural
greenhouse effect, the mean temperature would be about minus 18°C, and the
Earth would be uninhabitable (choose the topic Lower atmosphere if you want to
read more about the greenhouse effect).
Emitting greenhouse
gases in large amounts increases the concentration of these gases in the
atmosphere, which then increases the greenhouse effect so that more heat is
trapped by the atmosphere. This can increase the temperature of the atmosphere
and change the climate on Earth.
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