What Is Global Warming, Explained - Ahmad Afiq
Glaciers
are melting, sea levels are rising, cloud forests are dying, and wildlife is scrambling to keep pace. It has become
clear that humans have caused most of the past century's warming by releasing heat-trapping gases as we power our modern lives.
Called greenhouse gases, their levels are higher now than at any time in the last 800,000
years.
We often call
the result global warming, but it is causing a set of changes to the Earth's
climate, or long-term weather patterns, that varies from place to place. While
many people think of global warming and climate change as synonyms, scientists use “climate change”
when describing the complex shifts now affecting our planet’s weather and
climate systems—in part because some areas actually get cooler in the short term.
Climate
change encompasses not only rising average temperatures but also extreme weather events, shifting wildlife populations and
habitats, rising seas, and a range of other impacts. All of those changes are
emerging as humans continue to add heat-trapping greenhouse
gases to the
atmosphere, changing the rhythms of climate that all living things have come to
rely on.
What will we
do—what can we do—to slow this human-caused warming? How will
we cope with the changes we've already set into motion? While we struggle to
figure it all out, the fate of the Earth as we know it—coasts, forests, farms,
and snow-capped mountains—hangs in the balance.
Understanding the 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, hence the name.
Sunlight
shines onto the Earth's surface, where the energy is absorbed and then radiate
back into the atmosphere as heat. In the atmosphere, greenhouse gas molecules
trap some of the heat, and the rest escapes into space. The more greenhouse
gases concentrate in the atmosphere, the more heat gets locked up in the
molecules.
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 natural
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 (33 degrees
Celsius) 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 have gone up and down over the Earth's history, but they had
been fairly constant for the past few thousand years. Global average
temperatures had also stayed fairly constant over that time—until the past 150 years. Through the burning of fossil fuels
and other activities that have emitted large amounts of greenhouse gases,
particularly over the past few decades, humans are now enhancing the greenhouse
effect and warming Earth significantly, and in ways that promise many effects, scientists warn.
Aren't temperature changes natural?
Human
activity isn't the only factor that affects Earth's climate. Volcanic eruptions
and variations in solar radiation from sunspots, solar wind, and the Earth's
position relative to the sun also play a role. So do large-scale weather patterns such as El Niño.
But climate
models that scientists use to monitor Earth’s temperatures take those factors
into account. Changes in solar radiation levels as well as minute particles suspended in the atmosphere from
volcanic eruptions,
for example, have contributed only about two percent to the recent warming
effect. The balance comes from greenhouse gases and other human-caused factors, such as land use change.
The short
timescale of this recent warming is singular as well. Volcanic eruptions, for example, emit particles that
temporarily cool the Earth's surface. But their effect lasts just a few years.
Events like El Niño also work on fairly short and predictable cycles.
On the other hand, the types of global temperature fluctuations that have
contributed to ice ages occur on a cycle of hundreds of thousands of years.
For thousands
of years now, emissions of greenhouse gases to the atmosphere have been
balanced out by greenhouse gases that are naturally absorbed. As a result,
greenhouse gas concentrations and temperatures have been fairly stable, which
has allowed human civilization to flourish within a consistent climate.
Now, humans
have increased the amount of carbon dioxide in the atmosphere by more than a
third since the Industrial Revolution. Changes that have historically taken
thousands of years are now happening over the course of decades.
Why does this matter?
The rapid rise in greenhouse gases is a problem because it’s changing the
climate faster than some living things can adapt to. Also, a new and more
unpredictable climate poses unique challenges to all life.
Historically,
Earth's climate has regularly shifted between temperatures like those we see
today and temperatures cold enough to cover much of North America and Europe
with ice. The difference between average global temperatures today and during
those ice ages is only about 9 degrees Fahrenheit (5 degrees Celsius), and the
swings have tended to happen slowly, over hundreds of thousands of years.
But with
concentrations of greenhouse gases rising, Earth's remaining ice sheets such as
Greenland and Antarctica are starting to melt too. That extra water could raise sea
levels significantly, and quickly. By 2050, sea levels are predicted to rise between one and
2.3 feet as
glaciers melt.
As the mercury rises, the climate can change
in unexpected ways. In addition to sea levels rising, weather can become more extreme. This means more intense major
storms, more rain followed by longer and drier droughts—a challenge for growing
crops—changes in the ranges in which plants and animals can live, and loss of
water supplies that have historically come from glaciers.
Global Warming, Article from NGW.



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