作者: O. Kirner , R. Ruhnke , B.-M. Sinnhuber
DOI: 10.1080/07055900.2014.980718
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摘要: AbstractTo evaluate future climate change in the middle atmosphere and chemistry–climate interaction of stratospheric ozone, we performed a long-term simulation from 1960 to 2050 with boundary conditions Intergovernmental Panel on Climate Change A1B greenhouse gas scenario World Meteorological Organization Ab halogen using model ECHAM5/MESSy Atmospheric Chemistry (EMAC). In addition this standard five sensitivity simulations 2000 rerun files mentioned above. For these used same setup as but changed for carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O), ozone-depleting substances (ODS). first fixed mixing ratios CO2, CH4, N2O amounts 2000. each four other ...