Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.
AAAS Store

Site Tools

  • AAAS
  • Subscribe
  • Feedback

Site Search

Search Advanced

Science 18 March 2005:
Vol. 307. no. 5716, pp. 1769 - 1772
DOI: 10.1126/science.1106663

Reports

How Much More Global Warming and Sea Level Rise?

Gerald A. Meehl,* Warren M. Washington, William D. Collins, Julie M. Arblaster, Aixue Hu, Lawrence E. Buja, Warren G. Strand, Haiyan Teng

Two global coupled climate models show that even if the concentrations of greenhouse gases in the atmosphere had been stabilized in the year 2000, we are already committed to further global warming of about another half degree and an additional 320% sea level rise caused by thermal expansion by the end of the 21st century. Projected weakening of the meridional overturning circulation in the North Atlantic Ocean does not lead to a net cooling in Europe. At any given point in time, even if concentrations are stabilized, there is a commitment to future climate changes that will be greater than those we have already observed.

National Center for Atmospheric Research, Post Office Box 3000, Boulder, CO 80307, USA.

* To whom correspondence should be addressed. E-mail: meehl{at}ncar.ucar.edu

Read the Full Text


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
A rapid upward shift of a forest ecotone during 40 years of warming in the Green Mountains of Vermont.
B. Beckage, B. Osborne, D. G. Gavin, C. Pucko, T. Siccama, and T. Perkins (2008)
PNAS 105, 4197-4202
   Abstract »    Full Text »    PDF »
Physicians and the Environment.
P. S. Auerbach (2008)
JAMA 299, 956-958
   Full Text »    PDF »
How Much More Rain Will Global Warming Bring?.
F. J. Wentz, L. Ricciardulli, K. Hilburn, and C. Mears (2007)
Science 317, 233-235
   Abstract »    Full Text »    PDF »
Diversity and distribution of marine microbial eukaryotes in the arctic ocean and adjacent seas..
C. Lovejoy, R. Massana, and C. Pedros-Alio (2006)
Appl. Envir. Microbiol. 72, 3085-3095
   Abstract »    Full Text »    PDF »
Paleoclimatic evidence for future ice-sheet instability and rapid sea-level rise..
J. T. Overpeck, B. L. Otto-Bliesner, G. H. Miller, D. R. Muhs, R. B. Alley, and J. T. Kiehl (2006)
Science 311, 1747-1750
   Abstract »    Full Text »    PDF »
The Importance of Land-Cover Change in Simulating Future Climates.
J. J. Feddema, K. W. Oleson, G. B. Bonan, L. O. Mearns, L. E. Buja, G. A. Meehl, and W. M. Washington (2005)
Science 310, 1674-1678
   Abstract »    Full Text »    PDF »
Sea levels: abrupt events and mechanisms of change.
R. Edwards (2005)
Progress in Physical Geography 29, 599-608
   PDF »
Fine-scale processes regulate the response of extreme events to global climate change.
N. S. Diffenbaugh, J. S. Pal, R. J. Trapp, and F. Giorgi (2005)
PNAS 102, 15774-15778
   Abstract »    Full Text »    PDF »
Ice-Sheet and Sea-Level Changes.
R. B. Alley, P. U. Clark, P. Huybrechts, and I. Joughin (2005)
Science 310, 456-460
   Abstract »    Full Text »    PDF »
Contributions of past and present human generations to committed warming caused by carbon dioxide.
P. Friedlingstein and S. Solomon (2005)
PNAS 102, 10832-10836
   Abstract »    Full Text »    PDF »



ADVERTISEMENT
Click Me!

ADVERTISEMENT
Click Me!

To Advertise     Find Products