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Global Climate Change Digest A Guide to Information on Greenhouse Gases and Ozone Depletion Published July 1988 through June 1999
FROM VOLUME 10, NUMBER 7, JULY 1997
NEWS...
RESEARCH NEWS
Item #d97jul81
Particles cause warming? Aircraft measurements presented by Peter
Hobbs and colleagues at the AGU Spring Meeting show that large carbon
particles, which absorb radiation, far outnumbered the more reflective sulfate
particles in pollution plumes of the northeastern U.S. (See Eos, p. 260,
June 24, 1997.) Theoretically, such a particle mixture would increase global
warming, opposite to the conventional understanding of the impact of
anthropogenic particles on climate.
Item #d97jul82
UV trend? A new analysis of surface-based UV data in the U.S.
produces inconclusive results on any trend since 1974, concluding only that the
existing data (from the Robertson-Berger meter network) are unsuitable for
determining trends. (See Weatherhead paper, PROF. PUBS./OZONE DEPLETION/UV
MEASUREMENTS, this Global Climate Change Digest issue--July 1997.
Item #d97jul83
Methyl bromide is found to be removed by biological processes in the
ocean, reducing its estimated atmospheric lifetime to less than a year. (See
Yvon-Lewis paper in PROF. PUBS./OZONE DEPLETION/METHYL BROMIDE, this Global
Climate Change Digest issue--July 1997.)
Item #d97jul84
Ozone hole recovery: By watching changes in the vertical profile of
ozone, it may be possible to detect recovery of the Antarctic ozone hole as
early as the year 2008. (See Hofmann paper, PROF. PUBS./OZONE
DEPLETION/DISTRIBUTION AND TRENDS, this Global Climate Change Digest issue--July
1997.)
Item #d97jul85
Aircraft exhaust particles that can destroy stratospheric ozone and
alter the Earth's radiation balance can be minimized by reducing exhaust
emissions of SO3, new research shows. For the past 20 years, aircraft engine
designers have only been concerned with minimizing nitrogen oxides to protect
ozone. (See Kärcher paper, PROF. PUBS./OZONE DEPLETION/AIRCRAFT IMPACTS,
this Global Climate Change Digest issue--July 1997, and New
Scientist, p. 18, Feb. 15.)
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