Articles | Volume 15, issue 20
https://doi.org/10.5194/acp-15-11789-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-11789-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Implications of carbon monoxide bias for methane lifetime and atmospheric composition in chemistry climate models
GESTAR, Universities Space Research Association, Columbia, MD, USA
NASA Goddard Space Flight Center, Greenbelt, MD, USA
B. N. Duncan
NASA Goddard Space Flight Center, Greenbelt, MD, USA
E. A. Yegorova
NASA Goddard Space Flight Center, Greenbelt, MD, USA
Earth System Science Interdisciplinary Center, College Park, MD, USA
now at: Nuclear Regulatory Commission, Rockville, MD, USA
J. Kouatchou
NASA Goddard Space Flight Center, Greenbelt, MD, USA
Science Systems and Applications Inc., Lanham, MD, USA
J. R. Ziemke
NASA Goddard Space Flight Center, Greenbelt, MD, USA
GESTAR, Morgan State University, Baltimore, MD, USA
A. R. Douglass
NASA Goddard Space Flight Center, Greenbelt, MD, USA
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Latest update: 23 Nov 2024
Short summary
A low bias in carbon monoxide (CO) at northern latitudes is a common feature of chemistry climate models. We find that increasing Northern Hemisphere (NH) CO emissions or reducing NH OH concentrations improves the agreement with CO surface observations, but reducing NH OH leads to a better comparison with MOPITT. Removing model biases in ozone and water vapor increases the simulated methane lifetime, but it does not give the 20% reduction in NH OH suggested by our analysis of the CO bias.
A low bias in carbon monoxide (CO) at northern latitudes is a common feature of chemistry...
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