lmd_LEGACY1984_abstracts.html

1984 .

S. Joussaume, R. Sadourny, and J. Jouzel. A general circulation model of water isotope cycles in the atmosphere. Nature, 311:24-29, September 1984. [ bib | DOI | ADS link ]

H₂¹⁸O and HDO are important climatic tracers largely used to reconstruct continental palaeoclimates. The only thorough way to compare isotopic distributions in precipitation for modern and palaeoconditions is to simulate isotope cycles using atmospheric general circulation models. H₂¹⁸O and HDO cycles incorporated into our atmospheric general circulation model show good agreement between observed and predicted values for modern conditions.

S. Joussaume, I. Rasool, R. Sadourny, and J.-R. Petit. Simulation of desert dust cycles in an atmospheric general circulation model. Annals of Glaciology, 5:208-210, 1984. [ bib | ADS link ]

S. Joussaume, R. Sadourny, and J. Jouzel. Simulation of the HDO and H218O cycles in an Atmospheric general circulation model. Annals of Glaciology, 5:204-207, 1984. [ bib | ADS link ]