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U.S. skies harbor ozone destroyer.


U.S. Skies Harbor Ozone Destroyer

Scientists have discovered unexpectedly large concentrations of ozone-destroying chlorine monoxide Chlorine monoxide is a chemical compound with the formula ClO. It plays an important role in the process of Ozone Depletion. In the stratosphere, chlorine atoms react with ozone molecules to form chlorine monoxide and oxygen.

Cl + O3 → ClO + O2
 over the United States United States, officially United States of America, republic (2005 est. pop. 295,734,000), 3,539,227 sq mi (9,166,598 sq km), North America. The United States is the world's third largest country in population and the fourth largest country in area.  -- an ominous sign that chlorine pollution is thinning the ozone layer ozone layer or ozonosphere, region of the stratosphere containing relatively high concentrations of ozone, located at altitudes of 12–30 mi (19–48 km) above the earth's surface.  not just over the poles, but also over the densely populated midlatitudes.

"This is the first direct evidence we have at midlatitudes that chlorine compounds can destroy ozone during the wintertime," says Darin W. Toohey of Harvard University, who coauthored the report in the January GEOPHYSICAL RESEARCH LETTERS Geophysical Research Letters is a publication of the American Geophysical Union. GRL is the organization's only letters journal. Since its introduction in 1974, GRL has published only short research letters, typically 3-5 pages long, which focus on a specific discipline or .

Atmospheric scientists cannot yet gauge how much ozone destruction occurs over temperate regions. While the loss clearly remains small compared with the Antarctic "ozone hole," researchers worry that midlatitude depletions might accelerate dramatically during the next decade as atmospheric chlorine levels rise. Such ozone loss threatens humans and other life forms by allowing more ultraviolet radiation to reach Earth's surface.

Toohey and his co-workers describe measurements of chlorine monoxide made in 1988 and 1989 during a series of flights by NASA's high-altitude ER-2 research plane. This highly active form of chlorine is the main compound responsible for breaking apart ozone molecules over the poles. Scientists have dubbed it a "smoking gun" because elevated levels of the compound provide clear evidence that chlorine is destroying ozone. Most chlorine in the ozone layer comes from chlorofluorocarbons chlorofluorocarbons (klōr'əflr`əkär'bənz, klôr'–) (CFCs), organic compounds that contain carbon, chlorine, and fluorine atoms.  and other forms of pollution.

In flights over midlatitude regions during October and early December of 1988, the ER-2 measured normal chlorine monoxide levels of about 20 to 30 parts per billion at an altitude of 19 kilometers. But later in December, it detected double that concentration. And on Feb. 21, 1989, a flight from Virginia to California detected levels about five to 10 time higher than the October value. Even greater levels turned up the day before on a flight from Norway to Virginia.

"These are the largest concentrations of chlorine monoxide ever measured at midlatitudes," Toohey says.

The February levels, if they persisted for a month, could destroy as much as 2 percent of the ozone in an affected region, he calculates. While such slow destruction could not create an ozone hole over, say, New York New York, state, United States
New York, Middle Atlantic state of the United States. It is bordered by Vermont, Massachusetts, Connecticut, and the Atlantic Ocean (E), New Jersey and Pennsylvania (S), Lakes Erie and Ontario and the Canadian province of
, widespread increases in chlorine monoxide could gradually deplete de·plete
v.
1. To use up something, such as a nutrient.

2. To empty something out, as the body of electrolytes.
 ozone levels over the northern midlatitudes.

In fact, wintertime ozone values during the last two decades have dropped by 3 to 6 percent in the northern midlatitudes, according to satellite and ground-based measurements. While it's tempting to blame that decrease on chlorine pollution, scientists lack enough evidence to establish a causal link, says Michael Prather of NASA's Goddard Institute for Space Studies The NASA Goddard Institute for Space Studies (GISS), at Columbia University in New York City, is a component laboratory of NASA's Goddard Space Flight Center Earth-Sun Exploration Division and a unit of The Earth Institute at Columbia University.  in New York City New York City: see New York, city.
New York City

City (pop., 2000: 8,008,278), southeastern New York, at the mouth of the Hudson River. The largest city in the U.S.
. Because the ER-2 only gathered data on a few days, researchers remain unsure whether the chlorine monoxide elevations last for any length of time. Moreover, the plane could not make measurements higher in the stratosphere, where the bulk of the ozone layer lies.

The ER-2 data leave researchers puzzling over the compound's origin. According to standard chemical theories, chlorine above the midlatitudes should remain locked up in "safe," inactive forms.

One possible answer comes from Anne R. Douglass of the NASA NASA: see National Aeronautics and Space Administration.
NASA
 in full National Aeronautics and Space Administration

Independent U.S.
 Goddard Space Flight Center The Goddard Space Flight Center (GSFC) is a major NASA space research laboratory established on May 1, 1959 as NASA's first space flight center. GSFC employs approximately 10,000 civil servants and contractors, and is located approximately 6.5 miles northeast of Washington, D.C.  in Greenbelt, Md. In the same issue of GEOPHYSICAL RESEARCH LETTERS, she and her colleagues describe computer simulations suggesting that the ER-2's February flights passed through polar air enriched with chlorine monoxide.

Chlorine monoxide levels skyrocket over the poles during winter as the stratosphere gets cold enough to form icy cloud particles, which allow inactive chlorine to become active chlorine monoxide. A globe-circling wind stream called the polar vortex keeps this polar air from mixing with warmer air over the midlatitudes. But in February 1989, the vortex shifted toward the United States, and Douglass suggests that the ER-2 passed close to, if not through, the edge of the polar air. She adds, however, that her theory cannot account for the high chlorine monoxide values measured in late December, when the plane flew nowhere near the vortex.

This fall, scientists plan to launch a six-month project to study the stratosphere over the midlatitudes and the north polar region North Polar Region

See Polar Regions.
. ER-2 data collected during this period will indicate where high levels of chlorine monoxide exist and how long they persist. The project will also seek the cause of the ozone decrease over the midlatitudes in winter. Some researchers believe that blobs of polar air break off from the vortex, lowering ozone values in midlatitude regions as they carry the ozone-poor air southward. The abundant chlorine monoxide in this polar air would further deplete midlatitude ozone.

Others believe that very little polar air migrates toward the equator. Instead, they suggest that tiny droplets of atmospheric sulfuric acid sulfuric acid, chemical compound, H2SO4, colorless, odorless, extremely corrosive, oily liquid. It is sometimes called oil of vitriol. Concentrated Sulfuric Acid
 transform inactive chlorine into chlorine monoxide over the midlatitudes.
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No portion of this article can be reproduced without the express written permission from the copyright holder.
Copyright 1991, Gale Group. All rights reserved. Gale Group is a Thomson Corporation Company.

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Title Annotation:chlorine monoxide and other compounds
Author:Monastersky, Richard
Publication:Science News
Date:Feb 9, 1991
Words:772
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