% 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{Vogel:17488,
      author       = {Vogel, B. and Feck, T. and Grooß, J.-U. and Riese, M.},
      title        = {{I}mpact of a possible future global hydrogen economy on
                      {A}rctic stratospheric ozone loss},
      journal      = {Energy $\&$ environmental science},
      volume       = {5},
      issn         = {1754-5692},
      address      = {Cambridge},
      publisher    = {RSC Publ.},
      reportid     = {PreJuSER-17488},
      pages        = {6445 - 6452},
      year         = {2012},
      note         = {The authors gratefully acknowledge Piers Forster for giving
                      an introduction to the radiative transfer model RAD and for
                      helpful discussions about the radiative forcing
                      calculations. We would like to thank Karlheinz Nogai for
                      assisting with figures. The work by B. Vogel was partly
                      funded by the European Commission as part of the project "A
                      European Network for Atmospheric Hydrogen Observations and
                      Studies (EUROHYDROS)" under contract 036916.},
      abstract     = {The potential role of molecular hydrogen (H-2) as a future
                      alternative energy carrier has generated widespread
                      interest. The possible amount of additional hydrogen
                      emission into the atmosphere in a hydrogen-based economy
                      depends on future hydrogen production and leakage rates
                      throughout the complete process chain. However, the expected
                      emissions are highly uncertain. Based on the current
                      literature an upper limit is estimated. Additional hydrogen
                      emissions yield enhanced water vapor concentrations in the
                      stratosphere which will have an impact on stratospheric
                      temperatures and on polar ozone loss. Both stratospheric
                      water vapor and ozone are important drivers of climate
                      change. The potential environmental risks are described and
                      assessed to be low compared to the environmental benefits.},
      keywords     = {J (WoSType)},
      cin          = {IEK-7},
      ddc          = {690},
      cid          = {I:(DE-Juel1)IEK-7-20101013},
      pnm          = {Atmosphäre und Klima},
      pid          = {G:(DE-Juel1)FUEK491},
      shelfmark    = {Chemistry, Multidisciplinary / Energy $\&$ Fuels /
                      Engineering, Chemical / Environmental Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000301984200021},
      doi          = {10.1039/c2ee03181g},
      url          = {https://juser.fz-juelich.de/record/17488},
}