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lmd_Picon1987_bib.html

lmd_Picon1987.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:"Picon"  ' -c year=1987 -c $type="ARTICLE" -oc lmd_Picon1987.txt -ob lmd_Picon1987.bib /home/WWW/LMD/public/Publis_LMDEMC3.link.bib}}
@article{1987AdSpR...7..199P,
  author = {{Picon}, L. and {Desbois}, M. and {Sèze}, G.},
  title = {{Use of meteosat ISCCP B2 data for the study of interannual variations of climatic elements in Africa}},
  journal = {Advances in Space Research},
  year = 1987,
  volume = 7,
  pages = {199-202},
  abstract = {{Composite monthly images corresponding to West African rainy seasons of
1983, 1984, and 1985, have been constructed from ISCCP B2 Meteosat data.
Average and standard deviation images from thermal infrared and water
vapor channels are studied. In the thermal infrared, differences between
the three years appear principally in the mean structure of the ITCZ,
North-South extend, northward boundary, longitudinal variations of the
convection. In the water vapor channel, well defined ``dry'' areas
appear, showing the location and extent of subsidence regions on a large
scale. These locations and extents also vary from year to year.
}},
  doi = {10.1016/0273-1177(87)90146-3},
  adsurl = {http://adsabs.harvard.edu/abs/1987AdSpR...7..199P},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
@article{1987AdSpR...7..163K,
  author = {{Kayiranga}, T. and {Desbois}, M. and {Picon}, L.},
  title = {{Diurnal variations of convective cloudiness in tropical Africa observed with Meteosat ISCCP B2 data}},
  journal = {Advances in Space Research},
  year = 1987,
  volume = 7,
  pages = {163-166},
  abstract = {{Monthly composite images have been constructed from 8 times of the day
from the ISCCP B2 Meteosat data set. Average and standard deviation
images in IR and WV channels have been constructed at first. These
images allow to describe the mean diurnal cycle of convection over
Africa, and show that this cycle is strongly influenced by the
orography. Comparisons between two very different rainy seasons in West
Africa, 1983 and 1985, show some differences in the diurnal cycles.
}},
  doi = {10.1016/0273-1177(87)90140-2},
  adsurl = {http://adsabs.harvard.edu/abs/1987AdSpR...7..163K},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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