William Richard Peltier

William Richard Peltier, Ph.D., D.Sc. (hc) (born 1943), is a university professor of physics at the University of Toronto. He is director of the Centre for Global Change Science , principal investigator of the Polar Climate Stability Network , and the Scientific Director of Canada's largest supercomputer centre, SciNet . He is a fellow of the Royal Society of Canada and of the American Geophysical Union.

His research interests include: atmospheric and oceanic waves and turbulence, geophysical fluid dynamics, physics of the planetary interior, and planetary climate.

He is notable for his involvement in global glacial reconstructions from the last glacial maximum to present. He has been a major (or the primary) contributor to the global reconstructions ICE-3G,[1] ICE-4G,[2] ICE-5G (VM2),[3] and the upcoming ICE-6G (VM5) (in press). These models are important for the quantification of post-glacial rebound and late Pleistocene to Holocene variations in sea level.

Education

Teaching appointments

Honours and awards

See also

References

  1. Tushingham, A. M.; Peltier, W. R. (1991). "Ice-3G: A New Global Model of Late Pleistocene Deglaciation Based Upon Geophysical Predictions of Post-Glacial Relative Sea Level Change". Journal of Geophysical Research 96: 4497. Bibcode:1991JGR....96.4497T. doi:10.1029/90JB01583.
  2. Peltier, W. R. (1994). "Ice Age Paleotopography". Science 265 (5169): 195–201. Bibcode:1994Sci...265..195P. doi:10.1126/science.265.5169.195. PMID 17750657.
  3. Peltier, W.R. (2004). "Global glacial isostasy and the surface of the ice-age Earth: the ICE-5G (VM2) Model and GRACE". Annual Review of Earth and Planetary Sciences 32: 111. Bibcode:2004AREPS..32..111P. doi:10.1146/annurev.earth.32.082503.144359.
  4. "Gruppe 2: Fysikkfag (herunder astronomi, fysikk og geofysikk)" (in Norwegian). Norwegian Academy of Science and Letters. Retrieved 7 October 2010.

External links

This article is issued from Wikipedia - version of the Thursday, March 17, 2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.