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Jonathan M. Gregory is a climate modeller working on mechanisms of global and large-scale change in climate and sea level on multidecadal and longer timescales. He is currently a senior scientist in the Climate Division of NERC's National Centre for Atmospheric Science (NCAS-Climate), located in the Department of Meteorology at the University of Reading, and a Met Office Science Fellow in [delete: the climate-change group] climate change at the Hadley Centre.

A 2004 study, led by Gregory and published in the journal Nature, predicted that [delete: run-away melting of the Greenland ice sheet could start within 50 years] the Greenland ice sheet is likely to eliminated as a consequence of global warming, resulting in [delete: its total meltdown over the next 1000 years and] a rise in global sea-levels by 7 meters over the next 1000 years or more.[1][2]

He was a co-ordinating Lead Author of the IPCC 2001 Third Assessment Report chapter 11 Changes in Sea Level [1], and a contributing author to the [delete: SAR chapter] sea level chapter in the IPCC Second Assessment Report. Gregory was also a [delete: co-] Lead Author of the IPCC 2007 Fourth Assessment Report chapter 5 Observations: Oceanic Climate Change and Sea Level[3] and chapter 10 Global Climate Projections[4]. IPCC was a co-recipient (with Al Gore) of the 2007 Nobel Peace Prize for its work on climate change.[5]

In 2010 Jonathan Gregory was awarded an Advanced [delete: Fellowship] Grant by the European Research Council to carry out research on sea level change.[6][7] In addition to sea level change, Gregory has worked in recent years on climate sensitivity and predicted changes in the Atlantic meridional overturning circulation, among other subjects.

Selected publications

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  • [delete: White, N. J ., J. A. Church, and J. M. Gregory, 2005. Coastal and global averaged sea level rise for 1950 to 2000 Geophys. Res. Lett., 32, pg(s). L01601.]
  • [delete: Connolley, W. M ., J. M. Gregory, E. Hunke, and A. J. McLaren, 2004. On the consistent scaling of terms in the sea ice dynamics equation J. Phys. Oceanogr., 34, 7, pg(s). 1776-1780.]
  • add: Gregory, J. M. and M. Webb, 2008: Tropospheric adjustment induces a cloud component in CO2 forcing J. Climate, 21, 58-71, DOI: 10.1175/2007JCLI1834.1.
  • add: Gregory, J. M., K. W. Dixon, R. J. Stouffer, A. J. Weaver, E. Driesschaert, M. Eby, T. Fichefet, H. Hasumi, A. Hu, J. H. Jungclaus, I. V. Kamenkovich, A. Levermann, M. Montoya, S. Murakami, S. Nawrath, A. Oka, A. P. Sokolov, R. B. Thorpe, 2005: A model intercomparison of changes in the Atlantic thermohaline circulation in response to increasing atmospheric CO2 concentration Geophys. Res. Lett., 32, L12703, DOI: 10.1029/2005GL023209.
  • Gregory, J. M ., H. T. Banks, P. A. Stott, J. A. Lowe, and M. D. Palmer, 2004. Simulated and observed decadal variability in ocean heat content Geophys. Res. Lett., 31, L15312
  • Gregory, J. M ., P. Huybrechts and S. C. B. Raper, 2004. Threatened loss of the Greenland ice-sheet, Nature, 428, 6983, pg(s). 616.
  • Gregory, J. M ., O. A. Saenko and A. J. Weaver, 2003. The role of the Atlantic freshwater balance in the hyteresis of the meridional overturning circulation Climate Dynamics, 21, 7-8, pg(s). 707-717.
  • Gregory, J. M ., R. J. Stouffer, S. C. B. Raper, P. A. Stott and N. A.Rayner, 2002. An observationally based estimate of the climate sensitivity. Journal of Climate, 15, 22, pg(s). 3117-3121.
  • Church, J. A . and J. M. Gregory, 2001. Sea level change In: Encyclopedia of Ocean Sciences. J. H. Steele and K. K. Turekian eds. Academic Press, London
  • Gregory, J. M ., J. A. Church, G. J. Boer, K. W. Dixon, G. M. Flato, D. R. Jackett, J. A. Lowe, S. P. O'Farrell, E. Roeckner, G. L. Russell, R. J. Stouffer and M. Winton, 2001. Comparison of results from several AOGCMs for global and regional sea-level change 1900-2100. Climate Dynamics, 18, 3-4, pg(s). 225-240.

References

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