lmd_Sadourny1989.bib
@comment{{This file has been generated by bib2bib 1.95}}
@comment{{Command line: /usr/bin/bib2bib --quiet -c 'not journal:"Discussions"' -c 'not journal:"Polymer Science"' -c ' author:"Sadourny" ' -c year=1989 -c $type="ARTICLE" -oc lmd_Sadourny1989.txt -ob lmd_Sadourny1989.bib /home/WWW/LMD/public/Publis_LMDLEGACY.link.bib}}
@article{1989JFM...206..433F,
author = {{Farge}, M. and {Sadourny}, R.},
title = {{Wave-vortex dynamics in rotating shallow water}},
journal = {Journal of Fluid Mechanics},
year = 1989,
month = sep,
volume = 206,
pages = {433-462},
doi = {10.1017/S0022112089002351},
adsurl = {http://adsabs.harvard.edu/abs/1989JFM...206..433F},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
@article{1989GMS....52..159J,
author = {{Joussaume}, S. and {Jouzel}, J. and {Sadourny}, R.},
title = {{Simulations of the last glacial maximum with an atmospheric general circulation model including paleoclimatic tracer cycles}},
journal = {Washington DC American Geophysical Union Geophysical Monograph Series},
year = 1989,
volume = 52,
pages = {159-162},
abstract = {{Simulations of the Last Glacial Maximum have been performed with an
atmospheric general circulation model. We focus on a new approach of the
problem with the modeling of important climatic tracers: water isotopes
and desert dust particles. The mean dependency of the water isotope
content of precipitation with temperature is similar to the present-day
one, but can depart locally. The global amount of dust is little changed
for the ice age, but important changes are simulated over some regions.
}},
doi = {10.1029/GM052p0159},
adsurl = {http://adsabs.harvard.edu/abs/1989GMS....52..159J},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
