How Hot Will It Get?
No one knows for sure, but the potential perils of climate
change make it unwise for us to ignore the greenhouse effect
by JON KRAKAUER
Not so long ago, people talked about global warming in
apocalyptic terms--imagining the Statue of Liberty up to its
chin in water or an onslaught of tropical diseases in Oslo.
Recently, however, advances in our understanding of climate have
moved global warming from a subject for a summer disaster movie
to a serious but manageable scientific and policy issue.
Here's what we know. Since sunlight is always falling on the
earth, the laws of physics decree that the planet has to radiate
the same amount of energy back into space to keep the books
balanced. The earth does this by sending infrared radiation out
through the atmosphere, where an array of molecules (the best
known is carbon dioxide) form a kind of blanket, holding
outgoing radiation for a while and warming the surface. The
molecules are similar to the glass in a greenhouse, which is why
the warming process is called the greenhouse effect.
The greenhouse effect is nothing new; it has been operating ever
since the earth formed. Without it, the surface of the globe
would be a frigid -20°C (-4°F), the oceans would
have frozen, and no life would have developed. So the issue we
face in the next millennium is not whether there will be a
greenhouse effect, but whether humans, by burning fossil fuels,
are adding enough carbon dioxide to the atmosphere to change it
(and our climate) in significant ways.
You might think that, knowing what causes greenhouse warming, it
would be an easy matter to predict how hot the world will be in
the next century. Unfortunately, things aren't that simple. The
world is a complex place, and reducing it to the climatologist's
tool of choice--the computer model--isn't easy. Around almost every
statement in the greenhouse debate is a penumbra of uncertainty
that results from our current inability to capture the full
complexity of the planet in our models.
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