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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 7, NUMBER 2, FEBRUARY 1994
PROFESSIONAL PUBLICATIONS...
- EPRI/SCRIPPS SYMPOSIUM PAPERS
Item #d94feb27
Energy, 18(12),
Dec. 1993 (Pergamon Press), contains the following six papers
from the second symposium (Sep. 1992) on global warming sponsored
by the Electric Power Research Institute and Scripps Institution
of Oceanography. Roughly 40 experts have begun meeting annually
to discuss recent developments that are possibly controversial
and capable of adding insight to the topic. An introductory
article (pp. 1223-1227) by W. Nierenberg of Scripps gives helpful
background and context for each paper.
"Does Fossil Fuel Consumption Lead to Global
Warming?" S.E. Schwartz (Brookhaven Natl. Lab, Upton NY
11973), 1229-1248. The cooling influence of sulfate aerosols
produced by fossil fuel combustion may overwhelm warming from CO2
in the short term, but only because fossil fuel combustion has
rapidly increased recently. In the long term the warming effect
of CO2 is likely to dominate.
"Issues and Concerns about Global Atmospheric
Ozone," D.J. Wuebbles (Lawrence-Livermore Natl. Lab., POB
808, Livermore CA 94550), D.E. Kinnison, 1249-1262. Reviews
current scientific understanding and the responses that
governments are taking.
"Tide Gauges Measure Tectonic Movements," K.O. Emery
(Woods Hole Oceanog. Inst., Woods Hole MA 02543), D.G. Aubrey,
1263-1271. Gives a thorough evaluation of the many factors that
can influence observed sea level changes, which complicate the
detection of any general rise in sea level related to climate
change.
"Solar Activity Variations and Global Temperature,"
E. Friis-Christensen (Danish Meteor. Inst., Lyngbyvej 100, DK-210
Copenhagen, Denmark), 1273-1284. The author, who recently
published evidence of a correlation between the length of the
solar sunspot cycle and the observed global temperature record,
reviews previous work on the topic and presents further work of
his own.
"Evidence on the Climate Impact of Solar
Variations," S. Baliunas (Harvard Smithsonian Ctr. for
Astrophys.), R. Jastrow, 1285-1295. Observations of the sun and a
number of solar-type stars suggest a physical explanation for the
correlation discussed in the previous paper. Application of the
idea to the history of solar surface magnetic activity since the
Maunder minimum indicates that variations in solar irradiance are
capable of explaining the half-degree global warming observed
during the last 100 years. (This work and reactions to it are
discussed in a research news article in Science, pp.
1372-1373, Nov. 26, 1993.)
"Atmospheric CO2 Residence Time and the Carbon
Cycle," C. Starr (Electric Power Res. Inst., POB 10412, Palo
Alto CA 94303), 1297-1310. Explores a drastic departure from the
conventional approach to the global carbon cycle by dropping the
assumption that the increase in CO2 of the last 100 years is
solely due to anthropogenic sources. This leads to the conclusion
that only 19% of the observed increase is anthropogenic; the rest
is due to a change in the natural carbon cycle.
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