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JEG
: The Research Page
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Research Interests
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I am currently a post-doctoral researcher at the Georgia Institute of Technology, after finishing my PhD in November... this website needs a rebirth, which it will get soon... Broadly speaking, my research is concerned with the role of the Tropics in long-term climate change. The central actor of this game is of course the El Niño-Southern Oscillation (ENSO) phenomenon, whose behavior I strive to understand on decadal to millennial timescales. My current research project is "Constraining the tropical Pacific’s role in low-frequency climate change of the last millennium", with Kim Cobb, Michael Mann, Nick Graham, Mike Alexander and Martin Hoerling. |
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CV
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My curriculum vitae (in PDF, but not in Latin, be reassured)
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Publications
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Work done during my PhD thesis : Dissertation abstract (PDF)
Grand Dissertation in Technicolor : ENSO dynamics and the Earth's climate : from decades to Ice Ages (PDF, 8.7 Mb)
Work done during my Master's thesis at LOCEAN in Paris, France (Diplôme d'Etudes Approfondies, 2001) :
Work done during my second year at the Ecole Normale Supérieure (Maîtrise, 2000) as a visiting student at Lamont: Emile-Geay, J., M. A. Cane, N. Naik, R. Seager, A. C. Clement and A. van Geen, 2003: Warren revisited: Atmospheric freshwater fluxes and "Why is no deep water formed in the North Pacific ?". Journal of Geophysical Research - Oceans, 108(C6): 3178, doi: 10.1029/2001JC001058. PDF |
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Presentations
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Conference in Mathematical Geophysics, June 2004. Abstract European Geophysical Union, Vienna , April 2005. Abstract Cooperative Institute for Climate Applications and Research , September 2005. PDF American Geophysical Union, December 2005. PDF Conference in Mathematical Geophysics, June 2006. |
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| Data | DATA Data used in the PAGES newsletter article (link) :
The following files contain a table (1000 rows by 3 columns). The first column is time (years A.D.), the second is the forcing (W/m2) and the third is the model response, as described by the 100-member ensemble average of the NINO3 index over 1000-1999 A.D. forced by radiative anomalies in two cases :
(you need to specify a length of 150 000 years and 4 values per year (npy=4) ) |