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Crying In the Rain
A
funny thing happened in rural Virginia on June 25, 2003. There
was a spontaneous outbreak of tears. No, people weren’t crying
over the stock market (things are looking better, at the moment).
Nor were those tears shed over anything personal. The culprit
was air pollution; in particular, a massive burst of ozone
that for the first time in memory produced a 1960s-vintage,
L.A.-style eye-burner.
Things only get this bad when
volatile organic compounds react with the nitrogen oxides
produced by cars and industry in the presence of strong sunlight
and light winds. This relationship has been understood for
a quite some time. It was the basis for the original California
ozone regulations. What seems inexplicable is how such a phenomenon
could erupt in a rural, mid-Atlantic setting. What was different
about this year and the year before, or any prior year for
that matter?
NOx, NOx, Who’s There?
It wasn’t the oxides of nitrogen.
It doesn’t stand to reason that there was a sudden spike in
the number of polluting cars. Every new car sold replaces
an old beater, and produces an increment of relatively cleaner
air.
Nor did a host of new power plants spring up, overnight. Any
utility executive will tell you that it is years (sometimes
a decade or longer) from imagination of a power station to
production of electricity.
It certainly didn’t have its origin in an up-tick of economic
activity, as a quick scan of national, regional, or state
GDP will reveal.
What was different is this: thanks to an abundance of rainfall
and snowmelt, the mid-Atlantic states got greener than a craps
table in Atlantic City. Over much of the East coast, trees
are the largest source of the volatile hydrocarbons required
to produce smog. The trees produce two major precursors of
ozoneisoprene and terpenesin vast quantities (one
tree equals nine new cars). The more vegetal matter, the greater
the emissions. Remember Ronald Reagan being ridiculed for
his “killer trees” remark? He knew.
East Beats West
Nasty smogs like the June 2003 surprise used to be l’air du
jour for Los Angeles. Think back to the cover of Tim Buckley’s
“Greetings From L.A.” album (now only available as an expensive,
imported CD on Amazon.com). California cleaned up its act
by pioneering auto emission regulations. While things still
can get a little soupy out there, terrible and irritating
smogs have been pretty much engineered out of the L.A. Basin.
Fact is, the rest of us have adopted (either by law or default)
the same emission standards. So why were eyes burning on the
Right Coast? Like the bumper sticker says, “Trees are the
answer.”
While not devoid of trees, urban California by removing automobiles
and some industries as sources of volatile organic compounds
reduced a large fraction of its air pollution problem. But
the same isn’t true out East where conservation and forest
management have combined to produce a virtual jungle. There
is more abundant tree biomass along the eastern seaboard than
there has been for at least three hundred years. When viewed
from the air, Washington, Atlanta, Richmond and Charlotte
appear to have been chopped out of a very aggressive vegetative
cover only too willing to reclaim open space. Cities in the
Golden State were hacked out of open grassland.
According to Georgia Tech scientist Bill Chameides (1980),
about sixty percent of airborne VOCs in metro-Atlanta have
their origin in vegetation. In rural areas such as the eye-stung
region in June, the figure approaches 100 percent. No matter
how you slice it, the airborne load is substantial. In the
presence of a very small amount of nitrogen oxides, those
VOCs will combine under hot and undisturbed conditions to
produce nasty smog.
Water, Water Everywhere
According to the U.S. Department of Commerce, the East has
just experienced its wettest spring (March-May) in 109 years
of record keeping. There were a record number of days with
measurable rainfall totaling a Seattle-like twenty-two days
in May 2003. June wasn’t far behind. Together, May and June
are likely to combine for an all-time record in the number
of rainy daysa record that might stand for a century
or two.
Not only was it wet, there were an amazing number of cloudy
days. That combination produces abundant vegetation. You can
test the hypothesis at home. Put plants under a grow-light
(which produces a lot less photosynthetic light than does
the sun, thereby mimicking a cloudy day), water them well
and, voila, you will see a massive profusion of leaves. More
leaves mean more isoprene and, in some cases, more terpenes.
Add those in the presence of nitrogen oxides and you’ve got
the fixin’s for smog.
So, Who’s to Blame?
Our Green buddies are apt to blame President Bush for the
yucky air. They’ll point out that he recently rolled back
an Executive Order from late in the Clinton Administration
that would have created an additional increment of nitrogen
oxide reduction from East Coast power plants. That’s a nice
try, but it would take more than a few months (and probably
a decade or so) for those regs to produce anything that could
be measured. Judging from the lack of any visibility trends
in the Mid-Atlantic in recent years (see Figure
1), oftentimes there’s no palpable result. Failing to
pin the tail on the elephant, the same folks are apt to transfer
the blame to global warming exacerbated by Bush/Cheney distancing
from the tenets of the Kyoto Protocol. But that doesn’t pass
muster, either. The same places that were so wet darn near
set a precedent for the-coldest-spring-on-record, too.
It seems there was a new class of pollutant that made a lot
of rural Easterners cry on June 25th. Move over CO2, it was
rain!
Reference
Chameides, W.L., et al., 1988. The role
of biogenic hydrocarbons in urban photochemical smog: Atlanta
as a case study. Science, 241:1473-1475.
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Figure 1. Mean
visibility at Reagan National Airport (Washington, DC),
a typical mid-Atlantic airport location, shows no major
trends in the last quarter-century, despite changing regulations.
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