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Building 54, Room 1720, Massachusetts Institute of Technology,
Cambridge, MA 02139
The realistic physical functioning of the greenhouse effect is
reviewed, and the role of dynamic transport and water vapor is
identified. Model errors and uncertainties are quantitatively compared
with the forcing due to doubling CO2, and they are shown to
be too large for reliable model evaluations of climate sensitivities. The possibility of directly measuring climate sensitivity is reviewed. A direct approach using satellite data to relate changes in globally averaged radiative flux changes at the top of the atmosphere to naturally occurring changes in global mean temperature is described. Indirect approaches to evaluating climate sensitivity involving the
response to volcanic eruptions and Eocene climate change are also
described. Finally, it is explained how, in principle, a climate that
is insensitive to gross radiative forcing as produced by doubling
CO2 might still be able to undergo major changes of the
sort associated with ice ages and equable climates.
Proc. Natl. Acad. Sci. USA
Vol. 94,
pp. 8335-8342,
August 1997
Colloquium Paper
This paper was presented at a colloquium entitled "Carbon
Dioxide and Climate Change," organized by Charles D. Keeling, held
November 13-15, 1995, at the National Academy of Sciences, Irvine, CA.
Can increasing carbon dioxide cause climate change?
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