CHAPTER 10
A PIECE OF THE SKY
IS MISSING
[T]his goodly frame, the earth, seems to me a sterile promontory; this most excellent canopy, the air, look you, this brave o’erhanging firmament, this majestical roof fretted with golden fire, why, it appears no other thing to me than a foul and pestilent congregation of vapors.
WILLIAM SHAKESPEARE,
Hamlet, II, ii, 308 (1600–1601)
I’d always wanted a toy electric train. But it wasn’t until I was 10 that my parents could afford to buy me one. What they got me, secondhand but in good condition, wasn’t one of those bantamweight, finger-long, miniature scale models you see today, but a real clunker. The locomotive alone must have weighed five pounds. There was also a coal tender, a passenger car, and a caboose. The all-metal interlocking tracks came in three varieties: straight, curved, and one beautifully crossed mutation that permitted the construction of a figure-eight railway. I saved up to buy a green plastic tunnel, so I could see the engine, its headlight dispelling the darkness, triumphantly chugging through.
My memories of those happy times are suffused with a smell—not unpleasant, faintly sweet, and always emanating from the transformer, a big black metal box with a sliding red lever that controlled the speed of the train. If you had asked me to describe its function, I suppose I would have said that it converted the kind of electricity in the walls of our apartment to the kind of electricity that the locomotive needed. Only much later did I learn that the smell was made by a particular chemical—generated by the electricity as it passed through air—and that the chemical had a name: ozone.
The air all around us, the stuff we breathe, is made of about 20 percent oxygen—not the atom, symbolized as O, but the molecule, symbolized as O2, meaning two oxygen atoms chemically bound together. This molecular oxygen is what makes us go. We breathe it in, combine it with food, and extract energy. Ozone is a much rarer way in which oxygen atoms combine. It is symbolized as O3, meaning three oxygen atoms chemically bound together.
My transformer had an imperfection. A tiny electric spark had been sputtering away, breaking the bonds of oxygen molecules as they happened by:
O2 + energy → O + O
(The arrow means is changed into.) But solitary oxygen atoms (O) are unhappy, chemically reactive, anxious to combine with adjacent molecules—and they do:
O + O2 + M → O3 + M
Here, M stands for any third molecule; it doesn’t get used up in the reaction but is required to help it along. M is a catalyst. There are plenty of M molecules around, chiefly molecular nitrogen.
That’s what was going on in my transformer to make ozone. It also goes on in automobile engines and in the fires of industry, producing reactive ozone down here near the ground, contributing to smog and industrial pollution. It doesn’t smell so sweet to me anymore. The biggest ozone danger is not too much of it down here, but too little of it up there.
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It was all done responsibly, carefully, with concern for the environment. By the 1920s, refrigerators were widely perceived to be a good thing. For reasons of convenience, public health, the ability of producers of fruit, vegetables, and milk products to market at sizable distances, and tasty meals combined, everyone wanted to have one. (No more lugging blocks of ice; what could be bad about that?) But the working fluid, whose heating and cooling provided the refrigeration, was either ammonia or sulfur dioxide—poisonous and evil-smelling gases. A leak was very ugly. A substitute was badly needed—one that was liquid under the right conditions, that would circulate inside the refrigerator but would not hurt anything if the refrigerator leaked or was converted into scrap metal. For these purposes it would be nice to find a material that was also neither poisonous nor flammable, that doesn’t corrode, burn your eyes, attract bugs, or even bother the cat. But in all of Nature, no such material seemed to exist.
So chemists in the United States and Weimar and Nazi Germany invented a class of molecules that had never existed on Earth before. They called them chlorofluorocarbons (CFCs), made up of one or more carbon atoms to which are attached some chlorine and/or fluorine atoms. Here’s one:
(C for carbon, Cl for chlorine, F for fluorine.) They were wildly successful, far exceeding the expectations of their inventors. Not only did they become the chief working fluid in refrigerators, but in air conditioners as well. They found widespread applications in aerosol spray cans, insulating foam, and industrial solvents and cleansing agents (especially in the microelectronics industry). The most famous brand name is Freon, a trademark of DuPont. It was used for decades and no harm seemed ever to come from it. Safe as safe could be, everyone figured. That’s why, after a while, a surprising amount of what we took for granted in industrial chemistry depended on CFCs.
By the early 1970s a million tons of the stuff were manufactured every year. So, it’s the early 1970s, let’s say, and you’re standing in your bathroom, spraying under your arms. The CFC aerosol comes out in a fine deodorant-carrying mist. The propellant CFC molecules don’t stick to you. They bounce off into the air, swirl near the mirror, careen off the walls. Eventually, some of them trickle out the window or under the door and, as time passes—it may take days or weeks—they find themselves in the great outdoors. The CFCs bump into other molecules in the air, off buildings and telephone poles, and, carried up by convection currents and by the global atmospheric circulation, are swept around the planet. With very few exceptions, they do not fall apart and do not chemically combine with any of the other molecules they encounter. They’re practically inert. After a few years, they find themselves in the high atmosphere.
Ozone is naturally formed up there at an altitude of around 25 kilometers (15 miles). Ultraviolet light (UV) from the Sun—corresponding to the spark in my imperfectly insulated electric-train transformer—breaks O2 molecules down into O atoms. They recombine and reform ozone, just as in my transformer.
A CFC molecule survives at those altitudes on the average for a century before the UV makes it give up its chlorine. Chlorine is a catalyst that destroys ozone molecules but is not destroyed itself. It takes a couple of years before the chlorine is carried back into the lower atmosphere and washed out in rainwater. In that time, a chlorine atom may preside over the destruction of 100,000 ozone molecules.
The reaction goes like this:
O2 + UV light → 2O
2Cl [from CFCs] + 2O3 → 2ClO + 2O2
2ClO + 2O → 2Cl [regenerating the Cl] + 2O2
So the net result is:
2O3 → 3O2
Two ozone molecules have been destroyed; three oxygen molecules have been generated; and the chlorine atoms are available to do further mischief.
So what? Who cares? Some invisible molecules, somewhere high up in the sky, are being destroyed by some other invisible molecules manufactured down here on Earth. Why should we worry about that?
Because ozone is our shield against ultraviolet light from the Sun. If all the ozone in the upper air were brought down to the temperature and pressure around you at this moment, the layer would be only three millimeters thick—about the height of the cuticle of your little finger if you’re not fastidiously manicured. It’s not very much ozone. But that ozone is all that stands between us and the fierce and searing long-wave UV from the Sun.
The UV danger we often hear about is skin cancer. Light-skinned people are especially vulnerable; dark-skinned people have a generous supply of melanin to protect them. (Suntanning is an adaptation whereby whites develop more protective melanin when exposed to UV.) There seems to be some remote cosmic justice in light-skinned people inventing CFCs, which then give skin cancer preferentially to light-skinned people, while dark-skinned people, having had little to do with this wonderful invention, are naturally protected. There are ten times more malignant skin cancers reported today than in the 1950s. While part of this increase may be due to better reporting, ozone loss and increased UV exposure seem implicated. If things were to get much worse,
light-skinned people might be required to use special protective clothing during routine excursions out-of-doors, at least at highish altitudes and latitudes.
But increased skin cancer, while a direct consequence of enhanced UV, and threatening millions of deaths, is not the worst of it. Nor is the increased rate of eye cataracts. More serious is the fact that UV injures the immune system—the body’s machinery for fighting disease—but, again, only for people who go out unprotected into the sunlight. Yet, as serious as this seems, the real danger lies elsewhere.
When exposed to ultraviolet light, the organic molecules that constitute all life on Earth fall apart or make unhealthy chemical attachments. The most prevalent beings that inhabit the oceans are tiny one-celled plants that float near the surface of the water—the phytoplankton. They can’t hide from the UV by diving deep because they make a living through harvesting sunlight. They live from hand to mouth (a metaphor only—they have neither hands nor mouths). Experiments show that even a moderate increase in UV harms the one-celled plants common in the Antarctic Ocean and elsewhere. Larger increases can be expected to cause profound distress and, eventually, massive deaths.
Preliminary measurements of populations of these microscopic plants in Antarctic waters show that there has recently been a striking decline—up to 25 percent—near the ocean’s surface. Phytoplankton, because they’re so small, lack the tough UV-absorbing skins of animals and higher plants. (In addition to a set of cascading consequences in the oceanic food chain, the deaths of phytoplankton eliminates their ability to extract carbon dioxide from the atmosphere—and thereby adds to global warming. This is one of several ways in which the thinning of the ozone layer and the heating of the Earth are connected—even though they are fundamentally very different questions. The main action for ozone depletion occurs in the ultraviolet; for global warming, in the visible and infrared.)
But if increasing UV falls on the oceans, the damage is not restricted to these little plants—because they are the food of one-celled animals (the zooplankton), who are eaten in turn by little shrimplike crustaceans (like those in my glass world number 4210—the krill), who are eaten by small fish, who are eaten by large fish, who are eaten by dolphins, whales, and people. The destruction of the little plants at the base of the food chain causes the entire chain to collapse. There are many such food chains, on land as in water, and all seem vulnerable to disruption by UV. For example, the bacteria in the roots of rice plants that grab nitrogen from the air are UV-sensitive. Increasing UV may threaten crops and possibly even compromise the human food supply. Laboratory studies of crops at midlatitudes show that many are injured by increases in the near-ultraviolet light that is let through as the ozone layer thins.
In permitting the ozone layer to be destroyed and the intensity of UV at the Earth’s surface to increase, we are posing challenges of unknown but worrisome severity to the fabric of life on our planet. We are ignorant about the complex mutual dependencies of the beings on Earth, and what the sequential consequences will be if we wipe out some especially vulnerable microbes on which larger organisms depend. We are tugging at a planetwide biological tapestry and do not know whether one thread only will come out in our hands, or whether the whole tapestry will unravel before us.
No one believes that the entire ozone layer is in imminent danger of disappearing. We will not—even if we remain wholly obdurate about acknowledging our danger—be reduced to the antiseptic circumstance of the Martian surface, pummeled by unfiltered solar UV. But even a worldwide reduction in the amount of ozone by 10 percent—and many scientists think that’s what the present dose of CFCs in the atmosphere will eventually bring about—looks to be very dangerous.
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In 1974, F. Sherwood Rowland and Mario Molina of the Irvine campus of the University of California first warned that CFCs—some million tons per year were being injected into the stratosphere—might seriously damage the ozone layer. Subsequent experiments and calculations by scientists all over the world have supported their findings. At first certain confirmatory calculations suggested the effect was there, but would be less serious than Rowland and Molina proposed; other calculations suggested it would be more serious. This is a common circumstance for a new scientific finding, as other scientists try to find out how robust the new discovery is. But the calculations settled down more or less where Rowland and Molina said they would. (And in 1995 they would share the Nobel Prize in Chemistry for this work.)
DuPont, which sold CFCs to the tune of $600 million a year, took out ads in newspapers and scientific journals, and testified before Congressional committees that the danger of CFCs to the ozone layer was unproved, had been greatly exaggerated, or was based on faulty scientific reasoning. Its ads compared “theorists and some legislators,” who were for banning CFCs in aerosols, with “researchers and the aerosol industry,” who were for temporizing. It argued that “other chemicals … are primarily responsible” and warned about “businesses destroyed by premature legislative action.” It claimed a “lack of evidence” on the issue and promised to begin three years of research, after which they might do something. A powerful and profitable corporation was not about to risk hundreds of millions of dollars a year on the mere say-so of a few photochemists. When the theory was proven beyond the shadow of a doubt, they in effect said, that would be soon enough to consider making changes. Sometimes they seemed to be arguing that CFC manufacture would be halted as soon as the ozone layer was irretrievably damaged. But by then there might be no customers.
Once CFCs are in the atmosphere, there is no way to scrub them out (or to pump ozone from down here, where it’s a pollutant, to up there, where it’s needed). The effects of CFCs, once introduced into the air, will persist for about a century. Thus Sherwood Rowland, other scientists, and the Washington-based Natural Resources Defense Council urged the banning of CFCs. By 1978, CFC propellants in aerosol spray cans were made illegal in the United States, Canada, Norway, and Sweden. But most world CFC production did not go into spray cans. Public concern was temporarily mollified, attention drifted elsewhere, and the CFC content of the air continued to rise. The amount of chlorine in the atmosphere reached twice what it was when Rowland and Molina sounded the alarm and five times what it was in 1950.
For years, the British Antarctic Survey, a team of scientists stationed at Halley Bay in the southernmost continent, had been measuring the ozone layer high overhead. In 1985 they announced the disconcerting news that the springtime ozone had diminished to nearly half what they had measured a few years before. The discovery was confirmed by a NASA satellite. Two-thirds of the springtime ozone over Antarctica is now missing. There’s a hole in the Antarctic ozone layer. It has shown up every spring since the late 1970s. While it heals itself in winter, the hole seems to last longer each spring. No scientist had predicted it.
Naturally, the hole led to more calls for a ban on CFCs (as did the discovery that CFCs add to the global warming caused by the carbon dioxide greenhouse effect). But industry officials seemed to have difficulty focusing on the nature of the problem. Richard C. Barnett, chairman of the Alliance for a Responsible CFC Policy—formed by CFC manufacturers—complained: “The rapid, complete shutdown of CFCs that some people are calling for would have horrendous consequences. Some industries would have to shut down because they cannot get alternative products—the cure could kill the patient.” But the patient is not “some industries”; the patient might be life on Earth.
The Chemical Manufacturers Association believed that the Antarctic hole “is highly unlikely to have global significance.… Even in the other most similar region of the world, the Arctic, the meteorology effectively precludes a similar situation.”
More recently, enhanced levels of reactive chlorine have been found in the ozone hole, helping to establish the CFC connection. And measurements near the North Pole suggest that an ozone hole is developing over the Arctic as well. A 1996 study called “Satellite confirmation of the dominance of chloro
fluorocarbons in the global stratospheric chlorine budget” draws the unusually strong conclusion (for a scientific paper) that CFCs are implicated in ozone depletion “beyond reasonable doubt.” The role of chlorine from volcanos and sea spray—advocated by some right-wing radio commentators—accounts at most for 5 percent of the destroyed ozone.
At northern midlatitudes, where most people on Earth live, the amount of ozone seems to have been steadily declining at least since 1969. There are fluctuations, of course, and volcanic aerosols in the stratosphere work to decrease ozone levels for a year or two before they settle out. But to find (according to the World Meteorological Organization) 30 percent relative depletions over northern midlatitudes for some months of each year, and 45 percent in some areas, is cause for alarm. You don’t need many consecutive years like that before it’s likely that the life underneath the thinning ozone layer is getting into trouble.
Berkeley, California, banned the white CFC-blown-foam insulation used to keep fast foods warm. McDonald’s pledged replacement of the most damaging CFCs in its packaging. Facing the threat of government regulations and consumer boycotts, DuPont finally announced in 1988, 14 years after the CFC danger had been identified, that it would phase out the manufacture of CFCs—but not to be completed until the year 2000. Other American manufacturers did not then promise even that. The United States, though, accounted for only 30 percent of worldwide CFC production. Clearly, since the long-term threat to the ozone layer is global, the solution would have to be global as well.