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HARVARD GAZETTE ARCHIVES
Environmental Risk of Supersonic Jets Probed
By William J. Cromie
Gazette Staff
When a high-flying spy plane dove through the exhaust of a
Concorde supersonic jet flying tourists around the world, it produced
a scientific surprise. The exhaust contained an unexpectedly high number
of particles, a fact that bears on the protective ozone umbrella over our
heads and on global warming.
The startling discovery looms as a possible monkey wrench in the plans
of the U.S. and other nations to build supersonic commercial airliners that
will cut hours off a trip across the Pacific Ocean.
"Many people are trying to predict the effects of exhaust gases
and particles on the stratospheric ozone that protects us from harmful ultraviolet
radiation from the sun," says Steven Wofsy, Gordon McKay Professor
of Atmospheric and Environmental Sciences. "Computer models have been
developed in laboratories and many measurements made from research aircraft,
but this was the first time we obtained information about real airplanes
flying in the stratosphere."
"The results have made a lot of people nervous," continues
Paul Wennberg, a research associate in chemistry. "The surprising number
of particles are very tiny -- millionths of an inch in size. We have no
idea what they are made of, and they could alter our predictions of how
the new commercial aircraft will affect ozone levels and, perhaps, global
warming."
Four Hours to Tokyo
One thing Wofsy, Wennberg, and their Harvard colleagues know for certain:
there have been a lot of surprises in the stratosphere and there will probably
be many more. This cold, calm region of our atmosphere begins between 5
and 11 miles high, and extends up to roughly 30 miles. This transition area
between the turbulent, cloudy lower atmosphere and near-space contains the
ozone layer that shields us from the radiation that is implicated in skin
cancer, cataracts, and crop damage and other ecological calamities.
The U.S. runs a $500 million research program to investigate the feasibility
of the so-called High Speed Civil Transports (HSCT), which would pass through
the lower part of the stratosphere on their way to Asia, Europe, and Australia.
In one scenario, you could board a HSCT in Los Angeles in the morning and
arrive in Tokyo four hours later.
Before investing billions of dollars on these swift aircraft, however,
the airlines industry wants to know how the gases and particles they belch
out will affect the environment.
To find out, researchers from various universities and federal agencies
put instruments aboard National Aeronautics and Space Administration aircraft
that fly as high as 14 miles. These aircraft, formerly called U-2s and now
ER-2s, were designed for military spy missions. During the past four years
Wofsy's Harvard team has flown instruments on more than 100 flights, which
covered the stratosphere from the Arctic to the Antarctic at altitudes ranging
from 5 to 13 miles.
One goal of these high-in-the-sky missions is to determine how long gases
that rise from the turbulent lower atmosphere stay in the more stable stratosphere.
The team uses measurements of carbon dioxide, which comes from smokestacks
and tailpipes, to track air movements into and within the stratosphere
Their results were unexpected.
"We determined that such gases move upward in tropical areas and
spread rapidly into both the Northern and Southern Hemispheres," notes
Kristie Boering, a research associate in atmospheric chemistry. "They
stay in the stratosphere an average of five years before descending into
the middle latitudes and polar regions. The longer gases stay in the stratosphere,
the more pollutants from stratoliners may build up. We estimate that pollutant
concentrations from proposed aircraft flying in the stratosphere will be
25 to 100 percent greater than previously expected," Boering wrote
in a report published recently in the journal Science.
That sounds like bad news.
"Not necessarily," Boering counters. "It helps us to test
whether computer models that simulate the atmosphere are accurate. The models
are used to predict the consequences of increased levels of gas and particles,
natural and artificial, on ozone depletion and global warming. Our results
have already improved these computer simulations. If models and measurements
continue to agree, that will increase confidence in our predictions of the
impact of HSCT emissions."
Ozone Killers
Carbon dioxide is a major cause of global warming. High-flying stratoliners
probably won't spew out enough of the gas to make a big difference in the
lives of those living below, but nitrogen oxides, water vapor, and particles
of soot and sulfur in their exhausts might.
Another group, led by James Anderson, Weld Professor of Atmospheric Chemistry,
flies instruments on the same ER-2 flights to study chemical reactions that
can destroy ozone. Three years ago, they made measurements showing that
the chemistry of stratospheric ozone was radically different from what scientists
had believed since the early 1970s.
They had thought that nitrogen oxides, produced naturally and in airplane
exhaust, would be the principal killer of ozone. (These same noxious chemicals,
ejected from the tailpipes of cars and trucks, produce smog in Los Angeles
and other urban centers.) But measurements made by instruments aboard the
spy planes showed just the opposite. Nitrogen oxides were found to play
only a minor role in destroying ozone in the lower stratosphere. In fact,
these oxides take up other, more dangerous compounds, such as the highly
reactive chemicals that eat huge holes in the ozone layer over Antarctica.
"We found that small increases in nitrogen oxides slow ozone destruction
at altitudes where we expect the heaviest HSCT traffic," Wennberg says.
"However, at higher altitudes, above 13 miles, they will probably lead
to ozone loss because of differences in chemistry at these heights."
Flying below 12-13 miles won't solve the problem because, as Boering's
and Wofsy's research shows, gases emitted in the lower stratosphere make
their way to higher altitudes where they can chew up ozone.
Airlines don't want to order new aircraft if environmental regulations
might prevent them from flying. Before the first factory starts to build
the first stratoliners, the industry needs accurate computer models to predict
the impact of their exhausts. "The name of the game is prediction,"
says Wofsy.
"Fifteen years ago, such models were developed mainly on the basis
of laboratory studies," Wennberg comments. "After years of atmospheric
measurements and more recent lab work, they're becoming more precise. But
we still can't fully explain what's going on."
Frustrating gaps in knowledge remain. Most HSCT flights will be over
the Northern Hemisphere. Will the gases and particles from their exhaust
be concentrated in that hemisphere, or will they spread more or less evenly
over the entire globe? To answer that, Wofsy's team is preparing to launch
huge instrument-carrying helium balloons from Brazil into the high stratosphere.
ER-2 aircraft cannot fly higher than 14 miles; the balloons will extend
observations to about 18 miles.
Also, there are many questions about air movements and chemistry at the
bottom of the stratosphere, where many commercial airliners now fly. Anderson's
group is readying for the first measurements in this region, where, it is
suspected, highly reactive chemicals could effect global warming. Finally,
there's the nagging problem of those particles found in the wake of the
Concorde.
"It's increasingly clear that we know a lot more than we used to
know," says Wennberg, "but what we know isn't enough yet."
Copyright
1998 President and Fellows of Harvard College
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