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@ARTICLE{Chen:868422,
      author       = {Chen, Qiuyu and Kaufmann, Martin and Zhu, Yajun and Liu,
                      Jilin and Koppmann, Ralf and Riese, Martin},
      title        = {{G}lobal nighttime atomic oxygen abundances from {GOMOS}
                      hydroxyl airglow measurements in the mesopause region},
      journal      = {Atmospheric chemistry and physics},
      volume       = {19},
      number       = {22},
      issn         = {1680-7324},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {FZJ-2020-00025},
      pages        = {13891 - 13910},
      year         = {2019},
      abstract     = {This paper presents a new dataset of nighttime atomic
                      oxygen density [O], derived from OH(8–4) ro-vibrational
                      band emissions, using a non-local thermal equilibrium model,
                      with the aim of offering new insight into the atomic oxygen
                      abundances in the mesopause region. The dataset is derived
                      from the level-1 atmospheric background measurements
                      observed by the Global Ozone Monitoring by Occultation of
                      Stars (GOMOS) instrument aboard Envisat, with the Sounding
                      of the Atmosphere using Broadband Emission Radiometry
                      (SABER) measurements for the atmospheric background. Raw
                      data are reprocessed into monthly zonal mean values in 10∘
                      latitude bins with a fixed altitude grid of 3 km. The
                      dataset spans from 70∘ S to 70∘ N in latitude and
                      from 80 to 100 km in altitude, covering a time period from
                      May 2002 to December 2011 at local times from 22:00 to
                      00:00 LT.The atomic oxygen density peaks at about 95 km
                      and the highest values are in the range of
                      3–8 × 1011 atoms cm−3, depending on latitude
                      and season. There is a rapid decrease of [O] below the peak.
                      The annual oscillation (AO), semiannual oscillation (SAO)
                      and the solar cycle impact are distinguished from the [O]
                      longtime series variations. This new GOMOS [O] dataset
                      conforms to other published datasets and is consistent with
                      the [O] datasets obtained from the Scanning Imaging
                      Absorption Spectrometer for Atmospheric CHartographY
                      (SCIAMACHY) OH airglow measurements within about
                      $±20 \%.$},
      cin          = {IEK-7},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IEK-7-20101013},
      pnm          = {244 - Composition and dynamics of the upper troposphere and
                      middle atmosphere (POF3-244)},
      pid          = {G:(DE-HGF)POF3-244},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000498638500003},
      doi          = {10.5194/acp-19-13891-2019},
      url          = {https://juser.fz-juelich.de/record/868422},
}