% IMPORTANT: The following is UTF-8 encoded.  This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.

@ARTICLE{Lennartz:892647,
      author       = {Lennartz, Sinikka T. and Gauss, Michael and von Hobe, Marc
                      and Marandino, Christa A.},
      title        = {{M}onthly resolved modelled oceanic emissions of carbonyl
                      sulphide and carbon disulphide for the period 2000–2019},
      journal      = {Earth system science data},
      volume       = {13},
      number       = {5},
      issn         = {1866-3516},
      address      = {Katlenburg-Lindau},
      publisher    = {Copernics Publications},
      reportid     = {FZJ-2021-02233},
      pages        = {2095 - 2110},
      year         = {2021},
      abstract     = {Carbonyl sulphide (OCS) is the most abundant, long-lived
                      sulphur gas in the atmosphere and a major supplier of
                      sulphur to the stratospheric sulphate aerosol layer. The
                      short-lived gas carbon disulphide (CS2) is oxidized to OCS
                      and constitutes a major indirect source to the atmospheric
                      OCS budget. The atmospheric budget of OCS is not well
                      constrained due to a large missing source needed to
                      compensate for substantial evidence that was provided for
                      significantly higher sinks. Oceanic emissions are associated
                      with major uncertainties. Here we provide a first, monthly
                      resolved ocean emission inventory of both gases for the
                      period 2000–2019 (available at
                      https://doi.org/10.5281/zenodo.4297010) (Lennartz et al.,
                      2020a). Emissions are calculated with a numerical box model
                      (2.8°×2.8° resolution at the Equator, T42 grid) for the
                      oceanic surface mixed layer, driven by ERA5 data from ECMWF
                      and chromophoric dissolved organic matter (CDOM) from Aqua
                      MODIS. We find that interannual variability in OCS emissions
                      is smaller than seasonal variability and is mainly driven by
                      variations in CDOM, which influences both photochemical and
                      light-independent production. A comparison with a global
                      database of more than 2500 measurements reveals overall good
                      agreement. Emissions of CS2 constitute a larger sulphur
                      source to the atmosphere than OCS and equally show
                      interannual variability connected to variability in CDOM.
                      The emission estimate of CS2 is associated with higher
                      uncertainties as process understanding of the marine cycling
                      of CS2 is incomplete. We encourage the use of the data
                      provided here as input for atmospheric modelling studies to
                      further assess the atmospheric OCS budget and the role of
                      OCS in climate.},
      cin          = {IEK-7},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IEK-7-20101013},
      pnm          = {211 - Die Atmosphäre im globalen Wandel (POF4-211)},
      pid          = {G:(DE-HGF)POF4-211},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000653628200003},
      doi          = {10.5194/essd-13-2095-2021},
      url          = {https://juser.fz-juelich.de/record/892647},
}