b u s i n e s s

CASE GROWS FOR CLIMATE CHANGE New evidence leads to increasing concern that human-induced global warming from CO2 emissions is already here

Bette Hileman C&EN Washington

I n 1995, the United Nations Intergov­ernmental Panel on Climate Change declared: "The balance of evidence

suggests a discernible human influence on global climate." This conclusion set off a major battle among policymakers, scientists, and industry over the connec­tion between greenhouse gas emissions and global climate change.

That battle has continued, but in the four years since the UN report was re­leased, evidence for anomalous warm­ing has become more compelling, and as a result scientists have become more concerned that human-induced climate change has already arrived.

Data from many different fields now indicate that Earth is warming and that significant shifts are occurring in cli­mate and in the biosphere, at least in part because of human activities. How­ever, major uncertainties remain that make it difficult to predict the extent of warming or its consequences over the coming century.

Globally, almost every year since 1990 has been hotter than the preceding year, according to analysis from many studies. The average global surface temperature in 1998 was higher than in any year this century and was in fact higher than it has been at any time in the past 1,000 years. The tundra, which for millennia has stored large amounts of carbon in the form of peat, now seems to have become a net source of carbon dioxide emissions across vast areas of the Arctic.

Ocean temperatures during El Nino events since 1980 have been high enough to bleach corals in many regions, and much of that coral is diseased or dying. Because of strong warming, large sec­tions of the ice shelves on the Antarctic Peninsula—ice that has been stable for at least 400 years—have broken up recently.

Few scientists who publish research in the field of global warming believe these changes are entirely due to natural fluctuations in Earth's climate. Only a handful would say that human activi­ties—in particular, burning fossil fuels— have played no role in the global average 0.7 °C (1.2 °F) warming at ground level that has taken place since the late 1800s.

It is highly probable that the green­house gases added to the atmosphere since the start of the Industrial Revolu­tion have directly acted to heat up the planet and will heat it further over the coming century, says Jerry D. Mahl-man, director of the National Oceanic & Atmospheric Administration's (NOAA) Geophysical Fluid Dynamics Laborato­ry in Princeton, NJ.

However, scientists fall into two camps when they consider what society's

response to global warming should be. Some believe Earth's climate is already showing strong signs of instability and is causing alarming changes in sea ice and the biosphere. Consequently, they say governments and individuals need to take immediate action to curb emissions.

"Given the time frame over which these things, such as coral bleaching, are expressing themselves—decades, not centuries—we don't have time to take anything other than the precaution­ary principle as our appropriate role," says James W. Porter, a professor of ecology and marine sciences at the Uni­versity of Georgia, Athens. "The precau­tionary principle says, if the scientific evidence is incomplete, you shouldn't do anything to make the situation worse." The alternative, he says, should not be "if you don't understand every­thing, you should shut up and do nothing."

Other researchers believe there are some large uncertainties in global warming science that need to be elimi­nated or reduced before governments mandate strong, potentially expensive, measures to reduce emissions. "We need to take the steps now to make the political agreements and develop the technological capabilities to substantial­ly lower emissions if and when the sci­ence shows that to be necessary," says Ronald G. Prinn, director of the Center

Average global temperature in 1998 was higher than it has been for 1,000 years

Temperature change, 1.0

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-1.0 1000 1200 1400 1600 1800 2000

Temperature reconstruction from proxy data, such as tree rings and sediments Instrumental data Mean temperature (1902-80) 40-year running average temperatures from proxy data Linear trend (1000-1850)

Note: Yellow region indicates uncertainties, a Temperature change from the 1902-80 mean. Source: Geophys. Res. Lett., 26,759 (1999)

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for Global Change Science at Massa­chusetts Institute of Technology.

Several major questions dominate the unknowns of global warming science. These concern what effect clouds, aero­sols, ocean circulation, and vegetation (its uptake or emission of carbon dioxide) will have on global warming over the coming century. Another important question is: What kinds of regional changes in cli­mate might be expected as Earth warms? Satellite and ground-based instruments for the Earth Observing System that the National Aeronautics & Space Ad­ministration will deploy over the next 15 years are designed to help resolve these questions.

In recent international negotia­tions, the U.S. has advocated using reforestation and the incorporation of carbon in agricultural soils as a carbon dioxide sink to achieve a substantial part of the greenhouse gas emissions reductions agreed to under the 1997 Protocol to the United Nations Framework Con­vention on Climate Change— known as the Kyoto protocol. But many scientists and the European Union are skeptical about depending heavily upon this approach.

Evidence of warming Evidence pouring in from many differ­

ent fields indicates a speedup in the rise of Earth's surface temperature. Globally, 11 of the past 16 years have in turn been the hottest of the century, according to a NASA report The average global temper­ature in 1998 exceeded the previous record set in 1995 by 0.25 °C—a huge jump. The average global temperature in 1995 was already about 0.75 °C above temperatures during the late 1800s. Some of the warming in 1998 can be ex­plained by the El Nino phenomenon that year, but not most of it, says James E. Hansen, director of NASA's Goddard In­stitute for Space Studies in New York City. (El Nino is the periodic, marked warming of the central and eastern tropi­cal Pacific Ocean that can spawn droughts and floods worldwide.)

In addition, the rapid temperature rise of the past 25 years exceeds the rise seen in any previous period of equal length during the past century since reliable in­strumental data have been available. This accelerated warming has been occurring just as models have predicted—during the time when greenhouse gases in the atmo­sphere (about 80% carbon dioxide) have increased most rapidly, Hansen says.

When "proxy" records—such as tree rings, pollen, sediments, and gases trapped in glaciers—are used to esti­mate global temperatures in the distant past, 1998 stands out as a record hot year for the millennium, says Michael E. Mann, adjunct assistant professor of geosciences at the University of Massa­chusetts, Amherst The average global temperature last year exceeded tempera­tures in the so-called medieval warm peri­od, he says.

"The notion of

Mahlman (left) and Hansen

the medieval warm period is really out­dated," Mann says. Temperatures in Greenland were unusually high from about 900 to 1100, allowing the Norse col­onization, but that was a regional phe­nomenon, he explains. Europe warmed a few centuries later, but that warming was also confined to a small part of the planet 'There is no evidence of any period of warmth at the hemispheric scale that ri­vals the late 20th century," he explains.

Global temperatures in the late 20th century are a cause for concern, Mann says. "Any time a scientist sees a system exhibit very anomalous behavior all of a sudden, it is reason to be very cautious about whatever it is that might be per­turbing that system," he says. "There could be obviously deleterious and rela­tively unpredictable effects because we're changing the system so quickly."

As Earth's temperature has risen, most polar regions have warmed much more than the global average. Alaska, for example, has been as much as 6 °C (10 °F) warmer recently than it was 35 years ago, and this causes the Alaskan tundra to melt more in the summer than it used to.

It also means that vast areas of the tun­dra that formerly were a sink for carbon dioxide now have become net sources, according to Walter C. Oechel, director of the Global Change Research Group at San Diego State University. The tundra

has deep layers of peat that decay and re­lease carbon dioxide when warm.

Oechel has been measuring carbon dioxide emissions and absorption (flux) over an area about the size of the Neth­erlands on Alaska's North Slope. Using towers, chambers, and aircraft, he has found that essentially all of this area is now a net carbon dioxide source on an annual basis.

Measurements in the 1960s and early 1970s show that the Alaskan tun­dra was a carbon dioxide sink at that time, Oechel says. "The first year when we saw areas of the Arctic become sources during the summer was 1982," he says. From carbon-14 data for the peat, he concludes that "the tundra was basically a sink going back 9,000 years before present"

Oechel and several other re­search groups are extending flux studies to the Seward Peninsula in western Alaska and to the adja­cent Chukota Peninsula in Rus­sia. They are finding that the Rus­sian tundra also is a source. "The overall pattern is that the extrapo-

lar Arctic tundra is a source to the atmo­sphere," he says. "The two vegetation types we've looked at—tussock tundra and wet tundra—are emitting about 0.7 billion metric ton of carbon dioxide a year [measured as carbon]," he esti­mates, compared with about 7 billion metric tons released annually from burn­ing fossil fuels and from deforestation.

In addition to tundra, scientists are measuring how much C02 is emitted or absorbed by forests. Michael L Goulden, an assistant professor of earth system sci­ence at the University of California, Ir­vine, and his collaborators have been us­ing gas-exchange chambers; radiocarbon analysis; and wood, moss, and soil inven­tories to measure the carbon balance of a 120-year-old black spruce forest in Mani­toba. They found that the site has lost 0.3 metric ton of carbon per hectare per year from 1994 to 1997 [Science, 279, 214 (1998)]. The gain in wood carbon was more than offset by losses from the soil. "The soil remained frozen most of the year, and the decomposition of organ­ic matter in the soil increased 10-fold upon thawing," he writes.

Steven C. Wofsy, a professor of atmo­spheric and environmental science at Harvard University, has been measuring carbon fluxes in a variety of forests. Mea­surements made by Wofsy show that cer­tain types of boreal (high-latitude north-

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ern) forests are definitely not taking up any carbon, he says. But there aren't enough measurements yet to give a comprehensive picture of how much carbon dioxide boreal forests are ab­sorbing or emitting overall, he says. 'The atmospheric data, though, would suggest the boreal zone is not a very strong sink and may be a source today," Wofsy notes.

All this research shows that as cli­mate warms in the tundra or in the bore­al forests, it can transform them from sinks to sources.

Ice shelf breakup Average summertime temperatures

on the Antarctic Peninsula have risen 2.5 °C (4.5 °F) since the 1940s and are now just above 0 °C, according to data from the British Antarctic Survey. This strong warming seems to have led to in­creased colonization by plants at certain sites in the region and to have accelerat­ed the breakup of ice shelves on the peninsula. Two ice shelves, Larsen B and Wilkins, lost nearly 3,000 sq km (1,200 sq miles) of their total area of 24,000 sq km in the past year, according

to David Vaughan, a British Antarctic Survey researcher.

"We have evidence that the shelves in this area have been in retreat for 50 years," with cumulative losses amounting to about 7,000 sq km, he says. So retreat of 3,000 sq km in a single year is clear­ly an escalation, Vaughan says. The recent breakup was also unusual because the ice shelves calved thousands of small ice­bergs at once, while nor­mally they release only a few relatively large ice­bergs in any single year.

"Within a few years, much of the Wilkins Ice Shelf will likely be gone," Vaughan predicts. Al- Wofsy though the breakup and melting of an ice shelf does not contrib­ute to sea level rise because the shelf is originally floating on water, this phenom­enon has an important effect When an ice shelf is gone, the ice sheet (the huge glacier resting on land) behind the ice shelf would tend to melt faster because

New satellite network will aid climate-change research

The National Aeronautics & Space Ad­ministration's Earth Observing System (EOS) is a complex of satellites and ground-based instruments that will be deployed during the next 15 years. In all, there will be nearly 20 satellites, three of which have already been launched.

The flagship satellite of EOS, Terra, is scheduled for launch in October.

Terra will be equipped with five different instru­ments and is expected to provide the most useful information for under­standing global climate change.

Terra will be looking at Earth as a system. Its in­struments will measure atmospheric cloud radia­tive and microphysical properties, radiative en­ergy fluxes, methane, car­bon monoxide, aerosol optical properties, mois­ture, and temperature gradients. Terra also will measure such surface features as land cover and land use change, vege­tation dynamics, temperature, fire oc­currence, and volcanic effects. In addi­tion, Terra will collect data on sea sur­face temperature, phytoplankton in the

ocean, land ice and sea ice changes, and snow cover.

MISR (the Multiangle Imaging Spec-troRadiometer, pictured here and on the cover) is the most revolutionary instru­ment on Terra. Most satellite instru­ments look either straight down or to­ward the edge of the planet In contrast,

MISR will image Earth si­multaneously at nine dif­ferent angles in four color bands. It will be used to study clouds, Earth's sur­face, and aerosols—fea­tures that scatter light dif­ferently at different an­gles. MISR was built for NASA by the Jet Propul­sion Laboratory, Pasade­na, Calif.

V. (Ram) Ramanathan, director of the Center for Atmospheric Sciences at Scripps Institution of Oceanography, La Jolla, Calif., expects that Terra

will provide a tremendous amount of in­formation that will help eliminate uncer­tainties about aerosols, and will add a great deal to what is known about clouds. The effects of clouds and aerosols are still two of the big unknowns in climate-change science.

there is nothing to stop it from flowing out over the ocean, in what a NASA re­port calls an irreversible process.

The Greenland Ice Sheet, the world's second largest glacier, has begun to thin

by up to a meter per year when losses are averaged over the whole ice sheet, according to NASA sur­veys completed this year. In 1994, NASA researchers using aircraft equipped with laser altimeters mea­sured the profile of the 10 million-sq-km ice sheet This year, researchers flew on the same path and found that the ice sheet had lost up to 5 meters in thickness. The west side of the ice sheet had lost no net ice, but the east and

south sides had thinned substantially, leading to an overall loss. Significant melting of ice sheets would contribute to a sea level rise.

However, because snowfall could be increasing in polar regions, researchers still do not know whether the overall mass of all the world's polar ice sheets is growing or shrinking, NASA reports. There is no evidence yet that the huge ice sheet that covers the Antarctic conti­nent is thinning.

Coral bleaching Another effect believed to be caused

at least in part by the recent rise in glo­bal temperatures is that record seawa-ter temperatures have triggered the largest die-off of coral ever observed. "Worldwide episodes of coral bleach­ing, coral disease outbreaks, and macro algal overgrowth of coral are increas­ing in frequency, intensity, and range," says the University of Georgia's Porter. Bleaching occurs when coral becomes stressed and expels its microscopic plant life, which provides it food.

These events are occurring in all reef-supporting regions, including the Indo-Pacific, the western Atlantic, and the Car­ibbean, and are affecting reefs near both inhabited and uninhabited regions. Sci­entists attribute the coral decline to seven causes—coastal development, global warming, oxygen starvation, sediment loading (including dust from the Sahel, the semiarid fringe of the Sahara, in Afri­ca during drought years), destructive fishing practices, overfishing of plant-eat­ing fish, and increased ultraviolet radia­tion from stratospheric ozone depletion.

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But only global warming and en­hanced UV radiation are ubiquitous enough to affect coral globally in remote as well as inhabited areas, Porter says. Another clue to causality is that changes in the coral ecosystems started abruptly in the mid-1970s, just when global tem­peratures began rising rapidly, he says.

Coral bleaching has been particularly pronounced in El Nino years, especially during severe events, such as the one in 1998, Porter says. Since the mid-1970s, a number of very intense El Niiios have oc­curred when seawater temperatures have been unusually high, Porter says. If the water temperature rises to 31.5 °C, only 1.5 °C above the summertime sea-water average in the tropics, corals are bleached.

Coral can often recover from short bleaching episodes, but it becomes dis­eased or dies when subjected to pro­longed or repeated bleaching. Bleach­ing weakens coral's ability to resist pathogens or competitors, Porter says. "We are now seeing at least 14 diseases in coral, some of which appear to be new in that they have not been described be­fore," he says.

Porter currently is collaborating with the Environmental Protection Agency on long-term monitoring of coral reefs. In just three years, he has found a huge in­crease in the number of monitoring sta­tions in the Florida Keys with diseased coral. In 1996, there were 26 out of 160 EPA monitoring stations with disease. In 1998,131 stations exhibited disease. Fur­thermore, the number of coral species af­fected by disease in the Florida Keys has tripled over those three years. "No coral reef in Florida could have grown with the rates of loss now being seen," Porter says.

Reefs are threatened not only by ris­ing temperatures but also by the modi­fied chemical composition of the sur­face ocean water. Higher atmospheric concentrations of carbon dioxide result in enhanced absorption of carbon diox­ide by the surface ocean. This, in turn, lowers the concentration of carbonate ion, reducing the ability of corals to build their skeletons (made of calcium carbonate in the form of aragonite).

Joan A. Kleypas, a chemist at the Na­tional Center for Atmospheric Research (NCAR), Boulder, Colo., has found that the addition of extra carbon dioxide to surface ocean water has already reduced calcification rates on some reefs by 6 to 11% [Science, 284,118 (1999)]. She esti­mates that calcification rates would de­crease by an additional 8 to 17% if the car­

bon dioxide concentration in the atmo­sphere were to rise from its current level of 360 ppm to double the preindustrial level (about 550 ppm) as some models predict will happen by 2050.

Coral reefs are important because they are biologically diverse and beautiful marine ecosystems. They are important for tourism in many areas and provide food, coastal protection, and new medica­tions for drug-resistant diseases. For ex­ample, Caribbean countries derive half their gross national product from reefs, and the coral reefs of Southeast Asia har­bor onequarter of the world's fish species. The World Resources Institute, Washing­ton, D.C., estimates that the world's reefs provide $375 billion each year in goods and services.

An unstable climate At the same time that changes have

been taking place in coral, weather pat­terns have been shifting in ways that lead some scientists to believe that cli­mate has become unstable.

Thomas R Karl, director of NOAA's National Climatic Data Center, Asheville,

N.C., has analyzed weather records for the past century and found much evi­dence of an enhanced hydrological cycle. From his analysis, he concludes that pre­cipitation has increased about 10% across the contiguous U.S. since 1910, with much of the increase occurring in winter. Also, the proportion of total precipitation coming in very heavy events has risen relative to more moderate episodes, he says. For example, the frequency of ex­treme daily rainfall events (specifically, days with rainfall exceeding 2 inches) has increased by about 10% during the past century. Analyses of precipitation in Can­ada, Japan, Russia, China, and Australia show similar trends [Bull. Am. Meteorol. Soc, 79,231 (1998)].

Another sign of an enhanced hydro-logical cycle, Karl says, is that the mois­ture in the lower atmosphere in the U.S. has increased 5% per decade over the past 20 years. This is a consequence of simple physics: As temperatures rise, more water evaporates. Enhanced water vapor and increases in sulfate aerosols lead to more clouds, which tend to re­duce temperatures during the day and

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raise them at night. As a result, daily low temperatures in the U.S. have increased at nearly twice the rate of the daily highs. Similar trends can be seen in most other parts of the world.

Further evidence of an enhanced hy-drological cycle has been an increase in the number of intense storms over the North Atlantic and North Pacific Oceans, Karl says. This number has doubled since 1900.

In contrast, the frequency of tropical cyclones has decreased overall. This is not surprising, says Kevin E. Trenberth, chief of the climate analysis section at NCAR. "With increases in sea-surface temperatures, there is a potential for stronger, bigger hurricanes," he says. On the other hand, he explains, groups of thunderstorms can substitute for a hurri­cane as a mechanism to transport heat upward. So there is always a trade-off be­tween the two. However, it is very diffi­cult to detect trends in hurricanes be­cause they fluctuate so much from year to year.

For El Nino events, which are a major cause of widespread floods and droughts around the world, the trend is more clear-cut There have been more frequent and more intense El Ninos since the late 1970s, Trenberth says. The two most severe El Ninos on record occurred in 1982-83 and in 1997-98, and the longest on record persisted from 1990 to mid-1995.

There are reasons to think that global warming increases both the frequency and intensity of El Nino events, Tren­berth explains. "The timescale of El Nino is determined by the time required for an accumulation of warm water in the trop­ics to essentially recharge the system, plus the time for the El Nino itself to evolve. Because El Nino is in­volved with movement of heat "™ around, it is conceptually easy to see how increased heating from the buildup of greenhouse gases can interfere." As yet, however, there is no scientific consensus on how El Ninos are affected by ris­ing global temperatures.

Along with changes in the hy-drological cycle and in the El Nino phenomenon has come a sharp rise in the incidence of and damages from severe weather events around the world. Munich Re, a reinsurance company based in Munich, Germany, estimates that global losses from weather-related natural disasters have in­creased from between $7 billion

and $10 billion annually in the 1980s to about $90 billion annually in 1998.

Part of the reason damage costs have risen so much is that governments and insurers in developed countries have made inexpensive insurance widely available and this has encouraged peo­ple to build near the seacoast But at the same time the sheer number of severe weather events has also escalated.

Because of the ongoing climate changes, Karl says, effective future gov­ernment planning needs to account for a nonstationary climate. "We cannot rely on the past climate to guide us into the future," he says.

Models mimic reality There is no "smoking gun" in global

climate research that provides a near-absolute link between carbon dioxide emissions and climate change. But the newest general circulation models give results that, in the opinion of many scien­tists, come close to being a smoking gun. These models are very similar to those used for long-range weather forecasts.

In 1990, when general circulation models were used to project tempera­ture rises resulting from increasing greenhouse gases in the atmosphere, the modeled temperatures for the past century were not very close to the ob­served data. The models predicted a temperature rise of 1.2 °C from green­house gases during the 20th century, when the actual rise was about 0.7 °C.

But in 1995, when data on the cooling effects of sulfate aerosols and changes in the sun's irradiance were added to the models along with greenhouse gas­es, the model-predicted warming close­ly agreed with observations. There was

Losses from weather-related natural disasters up since 1990 $ Billions 100

1980 82 84

Source: Munich Re

also a close correspondence between model-predicted and observed patterns of temperature changes in the horizon­tal and vertical planes, says Tom M. L. Wigley, senior scientist at NCAR That is, the model-predicted temperature and precipitation patterns on continental and high-latitude/low-latitude scales were close to those seen in reality, he explains. Also, the pattern of tempera­tures predicted for different levels of the atmosphere was close to the measured pattern. "The skeptics' view that the models are inconsistent with observa­tions is just not correct," he says.

"If one takes off the shelf the best in­formation about greenhouse gas con­centrations, the best information about sulfate aerosol forcing (the warming or cooling result), the best information about solar forcing, and the best esti­mate about climate sensitivity (that is, how many watts per square meter of warming result from a given concentra­tion of greenhouse gases), then what you get" is very close to the observa­tions, Wigley explains.

Although the most sophisticated models give fairly realistic results for temperatures in the past, model predic­tions of the temperature changes to be expected in the next century vary wide­ly. Models project average global tem­perature increases of 1.2 to 4 °C com­pared with the 1990 global average if nothing is done to curb greenhouse gas­es. In Wigley's view, the best estimates range between 1.9 and 2.9 °C.

Some scientists say a global average temperature rise close to 1 °C—the low­est change projected for the next centu­ry—would have minimal effects. But Mann disagrees. A 1 °C global average

rise could have very noticeable —— effects on climate and the bio­

sphere because the rise in polar regions and even in the continen­tal U.S. would be much greater than 1 °C, he says.

One of the inputs that always makes temperature projections from climate models for the next century vary over a wide range is estimating how fast greenhouse gas concentrations will rise. That depends on many different human factors, including choices people make affecting population, chang­es in land use, and the structure of industry. It is impossible to elimi­nate all the uncertainties associat­ed with future human behavior.

Other large modeling uncer-

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tainties result from a lack of scientific understanding about the physical ef­fects of aerosols, clouds, and ocean cir­culation in a warmer world.

Aerosols—tiny particles suspended in air—originate from sea spray, volca­noes, dust storms, and wildfires, as well as fossil-fuel burning, ag­riculture, and forestry. Scientists do not know where on Earth aerosols are increasing or de­creasing. Nor do they under­stand how the effects of aerosols might change as greenhouse gas concentrations rise.

Preliminary results from a project to study aerosols over the Indian Ocean have produced many surprises and illustrate how little is known about aero­sols, says V. (Ram) Ramanathan, director of the Center for Atmo­spheric Sciences at Scripps Institution of Oceanography, La Jolla, Calif. In a National Science Foundation-sponsored project, scientists from Scripps and the Max Planck Institute for Chemistry, Mainz, Germany, used aircraft, ships, balloons, satellites, and land stations to study aerosols and clouds.

The aerosol layer—consisting of soot, sulfates, nitrates, and organics— was surprisingly persistent and thick and covered most of the Indian Ocean, Ramanathan says. A second unexpected finding was that the reduction of sun­light at the surface caused by the aero­sols was three times as great as the amount of sunlight the aerosols reflect­ed into space. Usually, the amount of sunlight reflected into space is the only measurement taken of the radiative properties of aerosols, he explains.

Another of the more important uncer­tainties in climate modeling is how the cloud system reacts in response to in­creases in the levels of greenhouse gas­es. In general, high clouds warm the cli­mate while low clouds, by reflecting sun­light back to space, tend to cool the system. Overall, clouds averaged togeth­er globally now have a net cooling effect of -15 to -20 watts per sq meter, Ramanathan says. However, scientists do not know how clouds will respond to further in­creases in greenhouse gases, he says.

NASA's Earth Observing System, which consists of satellite-based and ground-based instruments, is designed to reduce many of the uncertainties concern­ing clouds and aerosols. Data obtained will be used in complex Earth system models in climate projections for the next century

and to help in predicting regional changes in climate with increasing levels of green­house gases. A minimum of 15 years of continuous monitoring is believed to be needed to identi­fy meaningful cli-

Trenberth (left) and Karl

mate trends and to separate human effects from naturally occurring ones.

Insistence on sinks In the international negotiations over

what to do about the potential problems

of global climate change, beginning with those in Kyoto, the U.S. delegation has been advocating reforestation and the incorporation of carbon in agricul­

tural soils as a substitute for re­ducing emissions from burning fossil fuels. The U.S. aims to use sinks to achieve a substantial part of the 7% reduction in green­house gas emissions below the 1990 level by 2012 as promised in Kyoto. Government state­ments submitted to the UN by the State Department say that using sinks is often more eco­nomical than cutting back on the use of fossil fuel.

Although research on carbon sequestration in forests and soils had been going on for decades, the U.S. government did not seem to have an intense interest

in this topic until about the time of the Kyoto negotiations in December 1997. At that time, a draft paper by a group at NOAAs Geophysical Fluid Dynamics Laboratory was being circulated among the delegates. The paper, which was lat-

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er published in Science, concluded that the forests and soils of North America, especially those below the 51st parallel, were absorbing as much or more car­bon than the U.S. was emitting from burning fossil fuel [Science, 282, 442 (1988)].

According to the paper, North American forests and soils were sucking up 1.7 billion metric tons of carbon dioxide (measured as carbon) annual­ly—the entire so-called missing sink—while the rest of the world was taking up very little carbon dioxide. The paper was one rea­son U.S. policymakers came to believe that enhancing forest and soil carbon sequestration had great potential as an eco­nomical way to offset emissions reduction targets.

In Kyoto, delegates from the European Union believed that the U.S. interest in sinks had come out of the blue; they were very skeptical about in­cluding sinks in the protocol. At one point, the U.S. delegation threatened to walk out of the negotiations if sinks were not included.

In the past year, two more groups— one in Australia and one in France—have completed similar research and have come to differ­ent conclusions that show U.S. vegetation is taking up much less carbon dioxide than the NOAA researchers found. However, these new research results are not yet published and have had no noticeable effect on climate-change policy.

The sinks issue has been dom­inating every negotiating session since Kyoto, says Kevin R. Gur-ney, a research scientist in the department of atmospheric sci­ence at Colorado State Universi­ty, Fort Collins, who served as an expert at the negotiations. "A lot of the delegates are just per-plexed" because the issue is complicated and the science is not very mature, he explains. "It's difficult for them to negoti­ate issues that seem very vague and fuzzy."

But many scientists favor us­ing forest sinks as one way of re­ducing emissions under the pro­tocol. "The world would be a bet­ter place with more forests for many reasons—preservation of

biodiversity and production of forest products," says William H. Schlesinger, a professor of botany and geology at Duke University. He has been experi­menting with 13-year-old loblolly pine trees grown out­side to see how

Schlesinger (left) and Ramanathan

they respond to enhanced levels of car­bon dioxide. After three years, trees nourished with enhanced carbon diox­ide grew 25% faster than controls [Sci­ence, 284,1177 (1999)].

Schlesinger and his collaborators es­timate that if atmospheric carbon diox­ide levels double to 560 ppm sometime

Predicted temperatures are very close to those observed Temperature change, ° C a

1.21

1.0

0.8

0.6

0.4

0.2

-0 .2

n Greenhouse gases alone • Observed I Greenhouse gases + aerosols I Greenhouse gases + aerosols + solar irradiance

_ ] _ 1860 1880 1900 1920 1940 1960 1980 2000

a Change from the 1880-99 mean. Source: The Science of Climate Change" by Tom M. L. Wigley, published by Pew Center on Global Climate Change

When greenhouse gases, aerosols, and changes in solar irradiance are used as inputs into general cir­culation models, predicted temperatures are very close to those observed. When greenhouse gases are the only input, as was done in the past, predict­ed temperatures are higher than those observed.

in the next century as predicted, the world's forests could absorb 50% of the fossil-fuel emissions as an upper limit. But that would be an unrealistic goal, he says, achievable only if all the trees

were relatively young and all were as responsive to carbon di­oxide as the most responsive tree—the loblolly pine. Also, it is unclear whether the enhanced growth of trees would be sus­tained for more than a few years, he says.

Harvard's Wofsy also is in fa­vor of using forests and soils as a way to get credit for carbon diox­ide reductions. But, he says, people need to decide what the overall objectives are. These ob­jectives should put the manage­ment, stewardship, and ecologi­cal services of the forests and soils first and the advantages of

carbon reductions second, he believes. "A spreadsheet approach will lead to a big push from Wall Street to plant short-rotation, fast-growing tree plantations and ignore other environmental consid­erations," he says.

Widespread use of forests and soil sequestration as a substitute for reduc­

tions in fossil fuel use can back-fire, Gurney warns. "The prob­lem is that it's entirely possible every bit of carbon that goes into these systems now will come right out" as temperatures rise. To use sinks, he says, "you have to account for sink carbon forev­er, so if it comes out of forests or soils, countries [should be] pe­nalized for that."

Climate politics Some scientists believe Con­

gress is taking an ostrichlike ap­proach to climate-change issues. Last month, 50 climate-change researchers met in Washington, D.C., in an effort organized by the Union of Concerned Scien­tists to try to convince Congress that global warming is a serious issue and to urge the Senate to ratify the Kyoto protocol.

Since the Kyoto protocol was negotiated, Congress has for the most part been opposed to doing anything that might even­tually reduce greenhouse gas emissions. There has been some funding for research on climate change and for research

2 2 AUGUST 9,1999 C&EN

on nuclear and renewable energy, however.

There is virtually no chance the Senate will ratify the Kyoto proto­col during the Clinton Administra­tion. In fact, most members of Con­gress seem to agree with the view of Rep. Jim Sensenbrenner (R-Wis.) that the Kyoto protocol "pos­es a severe threat to the vitality of the U.S. economy in the form of drastic energy price increases, job losses in key manufacturing indus­tries, and an overall decline in our standard of living."

In March, Sen. John H. Chafee (R-R.I.) introduced S. 547, a bill to encourage companies to reduce their greenhouse gas emissions in re­turn for credits usable in any future cli­mate-change program. But this bill also has little chance of passage.

In April, Sen. Frank Murkowski (R-Alaska) introduced S. 882, a bill that would reduce and sequester greenhouse emissions through clean-coal technolo­gies, provide $2 billion over 10 years for R&D on various technologies that would reduce greenhouse gas emissions, and consolidate climate-change duties in one office at the Department of Energy. Envi­ronmental activists oppose Murkowski's bill, saying that while R&D is important, more immediate steps are necessary to reduce emissions.

Partly as a result of congressional in­action, the U.S. has made little progress toward meeting its goal of reducing greenhouse gas emissions 7% below the 1990 level by 2012. DOE's Energy Infor­mation Administration (EIA) has report­ed that U.S. emissions last year were more than 10% above the 1990 level.

EIA's 1998 emission figures also show that U.S. industry made some sur­prising progress last year in reducing carbon dioxide emissions. In 1998, fos­sil fuel use in the industrial sector fell 1.4% from the 1997 level, even as the gross domestic product grew 3.9%. This is the first time U.S. industrial use of fos­sil fuel has fallen in a strong economy. Emissions from 1997 to 1998 for the U.S. as a whole grew only 0.4%.

Perry Lindstrom, EIA industry econ­omist, says he does not know why in­dustrial emissions went down, nor does he know whether the trend will contin­ue. "Part of the downward movement has to be the result of a changing struc­ture in the U.S. economy," he says.

Similar trends can be seen around the world. Worldwide carbon emissions fell

Worldwide carbon dioxide emissions fell in 1998

U.S. China EU Russia Japan India

1998 C0 2 emissions (million metric tons

measured as carbon)

1,460 803 548 400 297 276

% change since 1990

10.3% 28.0

0.7a

-23.9b

5.6 55.2

% change 1997-98

0.4% -3.7 -0.9 -1.3 -2.5

1.8

WORLD 6,318 6.3 -0.5

a Change from 1991. b Change from 1992. Source: WorldWatch Institute (figures calculated from data supplied by BP Amoco and Oak Ridge National Laboratory)

0.5% last year while the world economy expanded 2.5%, according to figures from BP Amoco and the Worldwatch Institute, a Washington, D.C.-based public policy research organization. This shows there is a disconnect between economic expan­sion and carbon emissions, says Christo­pher Flavin, Worldwatch senior vice pres­ident. If that falling trend continues, it may demonstrate that cutting carbon

emissions and maintaining econom­ic growth may be easier than previ­ously thought

Research that casts light on glo­bal climate change is now published every week, and new data from NASA's Earth Observing System likely will provide much information that will help eliminate uncertain­ties over the next 10 to 15 years. Al­though the data may build an in­creasingly stronger case that green­house gases from the burning of fossil fuels are altering climate, they may never prove it absolutely.

So policy debates over whether the government should mandate major reductions in emissions now

or wait for more scientific certainty may well continue for a number of years. But eventually climate change and its asso­ciated harm to ecosystems may seem so ominous that a consensus among poli­cymakers, scientists, and the general public will develop to take strong mea­sures to reduce greenhouse gases, even while important scientific questions re­main unanswered.-^

Goodbye

Zones. e a s t m a n . c o m

commerce

AUGUST 9,1999 C&EN 2 3

Time