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On July 26, 1943,
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Los Angeles was blanketed by a thick
gas that stung people's eyes
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and blocked out the sun.
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Panicked residents believed their city
had been attacked using chemical warfare.
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But the cloud wasn't an act of war.
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It was smog.
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A portmanteau
of smock and fog,
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the word smog was coined at the beginning
of the 20th century
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to describe the thick gray
haze that covered cities
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such as London,
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Glasgow,
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and Edinburgh.
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This industrial smog was known to form
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when smoke from coal-burning
home stoves and factories
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combined with moisture in the air.
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But the smog behind
the LA panic was different.
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It was yellowish with a chemical odor.
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Since the city didn't burn much coal,
its cause would remain a mystery
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until a chemist named Arie Haagen-Smit
identified two culprits,
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volatile organic compounds, or VOCs,
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and nitrous oxides.
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VOCs are compounds that easily
become vapors
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and may contain elements, such as carbon,
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oxygen,
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hydrogen,
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chlorine,
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and sulfur.
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Some are naturally produced
by plants and animals,
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but others come from manmade sources,
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like solvents,
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paints,
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glues,
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and petrolleum.
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Meanwhile, the incomplete combustion
of gas in motor vehicles
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releases nitrous oxide.
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That's what gives this type of smog
its yellowish color.
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VOCs and nitrous oxide react with sunlight
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to produce secondary pollutants called
PANs and tropospheric,
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or ground level ozone.
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PANs and ozone cause eye irritation
and damage lung tissue.
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Both are key ingredients
in photochemical smog,
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which is what had been plaguing LA.
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So why does smog affect some cities
but not others?
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Both industrial and photochemical smog
combine manmade pollution
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with local weather and geography.
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London's high humidity made it a prime
location for industrial smog.
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Photochemical smog is strongest in
urban areas with calm winds
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and dry, warm, sunny weather.
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The ultraviolet radiation from sunlight
provides the energy necessary
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to breakdown molecules that contribute
to smog formation.
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Cities surrounded by mountains, like LA,
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or lying in a basin, like Beijing,
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are also especially vulnerable to smog
since there's nowhere for it to dissipate.
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That's also partially due to a phenomenon
known as temperature inversion,
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where instead of warm air
continuously rising upward,
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a pollution-filled layer of air remains
trapped near the Earth's surface
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by a slightly warmer layer above.
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Smog isn't just an aesthetic eyesore.
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Both forms of smog irritate the eyes,
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nose,
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and throat,
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exacerbate conditions like asthma
and emphysema,
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and increase the risk
of respiratory infections like bronchitis.
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Smog can be especially harmful
to young children and older people
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and exposure in pregnant women has been
linked to low birth weight
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and potential birth defects.
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Secondary pollutants found
in photochemical smog
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can damage and weaken crops
and decrease yield,
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making them more susceptible to insects.
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Yet for decades, smog was seen
as the inevitable price of civilization.
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Londoners had become accustomed to
the notorious pea soup fog
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swirling over their streets until 1952,
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when the great smog of London shut down
all transportation in the city for days
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and caused more
than 4,000 respiratory deaths.
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As a result, the Clean Air Act of 1956
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banned burning coal in
certain areas of the city,
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leading to a massive reduction in smog.
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Similarly, regulations on vehicle
emissions and gas content in the US
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reduced the volatile compounds in the air
and smog levels along with them.
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Smog remains a major problem
around the world.
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Countries like China and Poland that
depend on coal for energy
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experience high levels of industrial smog.
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Photochemical smog and airborne particles
from vehicle emissions
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affect many rapidly developing cities,
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from Mexico City and Santiago
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to New Delhi and Tehran.
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Governments have tried many methods
to tackle it,
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such as banning cars from driving
for days at a time.
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As more than half of the world's
population crowds into cities,
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considering a shift to mass transit
and away from fossil fuels
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may allow us to breath easier.