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1958: not a bad year for ozone.


Over the last decade, atmospheric scientists have gathered more than enough evidence to convict chlorofluorocarbons chlorofluorocarbons (klōr'əflr`əkär'bənz, klôr'–) (CFCs), organic compounds that contain carbon, chlorine, and fluorine atoms.  (CFCs) of creating the ozone hole over Antarctica. But that hasn't kept skeptics from trying to launch an appeal.

One point they frequently raise concerns a sketchy report of extremely low ozone readings over Antarctica in 1958, well before CFCs reached dangerous concentrations in the atmosphere. If accurate, such measurements would exonerate CFCs and recast the ozone hole as a natural phenomenon.

Although atmospheric scientists have long since written off these early low-ozone reports, researcher Paul A. Newman of NASA'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., decided to look at the 1950s data to settle the issue. In the April 22 SCIENCE, he concludes that "there is no credible evidence for an ozone hole in 1958."

The original readings came from French researchers who participated in the International Geophysical Year International Geophysical Year (IGY), 18-month period from July, 1957, through Dec., 1958, during a period of maximum sunspot activity, designated for cooperative study of the solar-terrestrial environment by the scientists of 67 nations.  in 1958 by performing experiments at the Dumont d'Urville station The Dumont d'Urville Station (French: Base Dumont d'Urville) is a French scientific station located in Antarctica on Île des Pétrels, archipelago of Pointe Géologie () in Adélie Land.  on the Antarctic coast. For one of their studies, they exposed spectrographic spec·tro·graph  
n.
1. A spectroscope equipped to photograph or otherwise record spectra.

2. A spectrogram.



spec
 plates to light from the moon, sun, and stars outside the solar system in order to gauge the amount of ultraviolet radiation reaching Earth's surface. Because atmospheric ozone blocks incoming ultraviolet light Ultraviolet light
A portion of the light spectrum not visible to the eye. Two bands of the UV spectrum, UVA and UVB, are used to treat psoriasis and other skin diseases.
, the French researchers used their data to infer the amount of ozone in the sky. They recorded concentrations as low as 110 Dobson units (DU) in September and 120 DU in October 1958.

Newman, however, reports that the Dumont d'Urville readings don't square with measurements taken at three other Antarctic sites and a fourth on a nearby island. Ozone amounts dipped no lower than 293 DU in October at these sites. Researchers there took measurements with the Dobson spectrophotometer spectrophotometer, instrument for measuring and comparing the intensities of common spectral lines in the spectra of two different sources of light. See photometry; spectroscope; spectrum. , a reliable and easy-to-operate tool still in use.

Newman regards the Dumont d'Urville readings as unreliable, for several reasons. Ozone readings at this site varied much more from day to day than did measurements at other locations in 1958. Furthermore, satellite measurements of the Dumont d'Urville area going back to 1978 suggest that the French data from 1958 do not match the typical ozone patterns observed in the region.
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Title Annotation:lack of evidence for ozone hole in 1958 suggests ozone hole may be a natural phenomenon
Publication:Science News
Date:May 21, 1994
Words:348
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