@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 year=1984 -c $type="ARTICLE" -oc lmd_EMC31984.txt -ob lmd_EMC31984.bib /home/WWW/LMD/public/Publis_LMDEMC3.link.bib}}
  author = {{Lemaitre}, M.-P. and {Laurent}, J. and {Besson}, J. and {Girard}, A. and 
	{Lippens}, C. and {Muller}, C. and {Vercheval}, J. and {Ackerman}, M.
  title = {{Sample Performance of the Grille Spectrometer}},
  journal = {Science},
  year = 1984,
  month = jul,
  volume = 225,
  pages = {171-172},
  abstract = {{The grille spectrometer observed the setting and rising sun 18 times
during the Spacelab 1 mission. In addition to solar absorption lines,
many of which had not been observed before, atmospheric spectral
absorptions due to carbon monoxide and carbon dioxide were observed at
heights tangent to the thermosphere (greater than 85 kilometers), and
absorptions due to ozone, water, methane, and nitrous oxide were
observed in the mesosphere (greater than 50 kilometers). The strongly
coupled molecules NO-NO$_{2}$ and HCl-HF were observed as pairs in
the stratosphere. Methane is presented as an example of the instrumental
operations because of the characteristic aspect of the Q branch of its
v$_{3}$ band.
  doi = {10.1126/science.225.4658.171},
  adsurl = {https://ui.adsabs.harvard.edu/abs/1984Sci...225..171L},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
  author = {{Lippens}, C. and {Muller}, C. and {Vercheval}, J. and {Ackermann}, M. and 
	{Laurent}, J. and {Lemaitre}, M.~P. and {Besson}, J. and {Girard}, A.
  title = {{Trace constituents measurements deduced from spectrometric observations on-board Spacelab}},
  journal = {Advances in Space Research},
  keywords = {Absorption Spectra, Atmospheric Composition, Carbon Dioxide Concentration, Infrared Spectroscopy, Spacelab Payloads, Trace Elements, Atmospheric Density, Carbon Monoxide, Infrared Absorption, Middle Atmosphere, Water Vapor},
  year = 1984,
  volume = 4,
  pages = {75-79},
  abstract = {{Spectrometric measurements of carbon dioxide, carbon monoxide, and water
vapor content in the middle atmosphere, obtained during the Spacelab
mission, are examined. The carbon dioxide volume mixing ratio obtained
follows closely the 0.0003 value up to a 100-km altitude, and drops
abruptly at higher altitudes by a factor of 10 (at 115 km). The results
of two absorption runs for carbon monoxide indicate a P(6) line at
sunset in the Northern Hemisphere. Finally, the water vapor content
studies in the spectral region of 6.3 and 2.7 microns suggest a tendency
for the water vapor mixing ratio abundance to increase with the altitude
increasing from 30 to 50 km and to decrease from 72 to 80 km.
  doi = {10.1016/0273-1177(84)90432-0},
  adsurl = {https://ui.adsabs.harvard.edu/abs/1984AdSpR...4...75L},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}