we've already set into motion? While
we struggle to figure it all out, the face
of the Earth as we know it—coasts,
forests, farms and snow-capped
mountains—hangs in the balance.
Greenhouse effect
The "greenhouse effect" is the
warming that happens when certain
gases in Earth's atmosphere trap heat.
These gases let in light but keep heat
from escaping, like the glass walls of a
greenhouse. First, sunlight shines
onto the Earth's surface, where it is
absorbed and then radiates back into
the atmosphere as heat. In the
atmosphere, “greenhouse” gases trap
some of this heat, and the rest
escapes into space. The more
greenhouse gases are in the
atmosphere, the more heat
gets trapped. Scientists have known
about the greenhouse effect since
1824, when Joseph Fourier calculated
that the Earth would be much colder if
it had no atmosphere. This
greenhouse effect is what keeps the
Earth's climate livable. Without it, the
Earth's surface would be an average
of about 60 degrees Fahrenheit
cooler. In 1895, the Swedish chemist
Svante Arrhenius discovered that
humans could enhance the
greenhouse effect by making carbon
dioxide, a greenhouse gas. He kicked
off 100 years of climate research that
has given us a sophisticated
understanding of global warming.
Levels of greenhouse gases (GHGs)
have gone up and down over the
Earth's history, but they have been
fairly constant for the past few
thousand years. Global average
temperatures have stayed fairly
constant over that time as well, until
recently. Through the burning of fossil
fuels and other GHG emissions,
humans are enhancing the
greenhouse effect and
warming Earth.
Scientists often use the term "climate
change" instead of global warming.
This is because as the Earth's
average temperature climbs, winds
and ocean currents move heat around
the globe in ways that can cool some
areas, warm others, and change the
amount of rain and snow falling. As a
result, the climate changes differently
in different areas
Aren’t temperature changes natural?
The average global temperature and
concentrations of carbon dioxide (one
of the major greenhouse gases) have
fluctuated on a cycle of hundreds of
thousands of years as the Earth's
position relative to the sun has varied.
As a result, ice ages have come and
gone. However, for thousands of
years now, emissions of GHGs to the
atmosphere have been balanced out
by GHGs that are naturally absorbed.
As a result, GHG concentrations and
temperature have been fairly stable.
This stability has allowed human
civilization to develop within a
consistent climate. Occasionally, other
factors briefly influence global
temperatures. Volcanic eruptions, for
example, emit particles that
temporarily cool the Earth's surface.
But these have no lasting effect
beyond a few years. Other
cycles, such as El Niño, also work on
fairly short and predictable cycles.
Now, humans have increased the
amount of carbon dioxide in the
atmosphere by more than a third since
the industrial revolution. Changes
this large have historically taken
thousands of years, but are now
happening over the course of
decades.