lmd_EMC31972.bib

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@article{1972Natur.240..300A,
  author = {{Ackerman}, M. and {Muller}, C.},
  title = {{Stratospheric Nitrogen Dioxide from Infrared Absorption Spectra}},
  journal = {\nat},
  year = 1972,
  month = dec,
  volume = 240,
  pages = {300-301},
  abstract = {{STRATOSPHERIC absorption due to NO$_{2}$ has been
identified$^{1-3}$ in infrared spectra of the solar radiation
recorded from balloon borne gondolas floating at mid-latitudes in the
altitude range of 30 km when the solar zenith angle is larger than
91{\deg}. In this particular geometric situation most of the absorption
by the atmosphere takes place at altitudes smaller than float altitude
over very long optical paths. This offers two great advantages: the
sensitivity of the absorption method is maximum and the quantitative
interpretation is easier because absorption takes place mostly at
constant total pressure, constituent concentration and temperature where
the solar radiation passes closest to the Earth's surface.
}},
  doi = {10.1038/240300a0},
  adsurl = {https://ui.adsabs.harvard.edu/abs/1972Natur.240..300A},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}