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Unit 8 Focus on Global Warming
John Weier
Twenty-five
years
ago
if
you
made
a
trip
to
the
local
library
and
perused
the
periodical section for articles on
global warming, you’d probably have come up with
only
a
few
abstracts
from
hardcore
science
journals
or
maybe
a
blurb
in
some
esoteric
geopolitical magazine. As an Internet
search on global warming now attests, the subject
has become as rooted in our public
consciousness as Madonna
2
or
microwave cooking.
1
Perhaps all this attention is deserved.
With the possible exception of another world
war,
giant
asteroid,
or
an
incurable
plague,
global
warming
may
be
the
single
largest
threat to our
planet.
2
For decades human
factories and cars have spewed billions of tons
of greenhouse gases into the
atmosphere, and the climate has begun to show some
signs
of
warming.
Many
see
this
as
a
harbinger
of
what
is
to
come.
3
If
we
don’t
curb
our
greenhouse gas emissions, then low-
lying nations could be awash in seawater, rain and
drought patterns across the world could
change, hurricanes could become more frequent,
and El Ninos could become more intense.
Our Warming Planet
What
has
worried
many
people
now
is
that
over
the
past
250
years
humans
have
been
artificially
raising
the
concentration
of
greenhouse
gases
in
the
atmosphere.
Our
factories, power plants, and cars burn
coal and gasoline and spit out a seemingly endless
stream
of
carbon
dioxide.
We
produce
millions
of
pounds
of
methane
by
allowing
our
trash to decompose in landfills and by
breeding large herds of methane-belching cattle.
Nitrogen-based
fertilizers,
which
we
use
on
nearly
all
our
crops,
release
unnatural
amounts of nitrogen oxide into the
atmosphere.
Once these carbon-based
greenhouse gases get into the atmosphere, they
stay there
for
decades
or
longer.
According
to
the
Intergovernmental
Panel
on
Climate
Change
(IPCC)
since
the
industrial
revolution,
carbon
dioxide
levels
have
increased
31
percent
and methane levels
have increased 151 percent. Paleoclimate readings
taken from fossil
records show that
these gases, two of the most abundant greenhouse
gases, are at their
highest
levels
in
the
past
420,000
years.
Many
scientists
fear
that
the
increased
concentrations
of
greenhouse
gases
have
prevented
additional
thermal
radiation
from
leaving
the
Eart
h.
In
essence,
these
gases
are
trapping
excess
heat
in
the
Earth’s
atmosphere in much
the same way that a windshield traps solar energy
that enters a car.
4
Much
of
the
available
climate
data
appear
to
back
these
fears.
5
Temperature
data
gathered
from
many
different
sources
all
across
the
globe
show
that
the
surface
temperature
of
the
Earth,
which
includes
the
lower
atmosphere
and
the
surface
of
the
ocean, has
risen dramatically over several decades. Worldwide
measurements of sea level
show a rise
of 0.1
to 0.2 meters over the last
century. That’s an increase of roughly
1
℃
every
4,000
years.
Readings
gathered
from
glaciers
reveal
a
steady
recession
of
the
world’s
continental
glaciers.
Taken
together,
all
of
these data
suggest
that
over
the
last
century the planet has
experienced the largest increase in surface
temperature
in 1,000
years.
Not
surprisingly,
many
scientists
speculate
that
such
changes
in
the
climate
will
probably result in hotter days and
fewer cool days.
6
According
to the IPCC, land surface
areas will
increase in temperature over the summer months
much more than the ocean.
The
mid-latitude
to
high-latitude
regions
in
the Northern
Hemisphere
—
areas
such
as
the
Continental United
States, Canada,
and
Siberia
—
will
likely warm
the most.
These
regions could exceed mean global
warming by as much as 40 percent.
As
far as human health is concerned, those hit
hardest will probably be residents of
poorer countries that do not have the
funds to fend against changes in
climate.
7
A slight
increase
in
heat
and
rain
in
equatorial
regions
would
likely
spark
an
increase
in
vector-borne
diseases
such
as
malaria.
More
intense
rains
and
hurricanes
could
cause
more
severe
flooding
and
more
deaths
in
coastal
regions
and
along
riverbeds.
Even
a
moderate rise in sea level could
threaten the coastlines of low-lying islands such
as the
Maldives. All across the globe,
hotter summers could lead to more cases of
heatstroke and
deaths among those who
are vulnerable, such as older people with heart
problems. The
warmer temperatures may
also lead to higher levels of near-surface ozone
from cars and
factories, which would
likely cause more perilous air quality days and
hospital admissions
for those with
respiratory problems.
Taking Actions
Fortunately,
we
can
take
actions
to
slow
down
global
warming.
8
Global
warming
results primarily from human activities
that release heat-trapping gases and particles
into
the air. The most important causes
include the burning of fossil fuels such as coal,
gas,
and
oil,
and
deforestation.
To
reduce
the
emission
of
heat-
trapping
gases
like
carbon
dioxide, methane,
and
nitrous
oxides,
we
can
curb
our
consumption of
fossil
fuels, use
technologies
that
reduce
the
amount
of
emissions
wherever
possible,
and
protect
the
forests in the world.
We
can also do things to mitigate the impacts of
global warming and adapt to those
most
likely to occur,
9
e.g.,
through careful planning and other strategies that
reduce our
vulnerability to global
warming.
But
we
can’t
stop
there.
We
are
also
advocating
policies
that
will
combat
global
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