Articles | Volume 16, issue 9
Atmos. Chem. Phys., 16, 5853–5866, 2016
https://doi.org/10.5194/acp-16-5853-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 16, 5853–5866, 2016
https://doi.org/10.5194/acp-16-5853-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
13 May 2016
Research article
| 13 May 2016
Atmospheric changes caused by galactic cosmic rays over the period 1960–2010
Charles H. Jackman et al.
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Cited
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- Hemispherical Asymmetry of the Lower Stratospheric O3 Response to Galactic Cosmic Rays Forcing N. Kilifarska 10.1021/acsearthspacechem.6b00009
- Cosmic Noise Absorption During Solar Proton Events in WACCM‐D and Riometer Observations E. Heino et al. 10.1029/2018JA026192
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- Solar forcing for CMIP6 (v3.2) K. Matthes et al. 10.5194/gmd-10-2247-2017
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- The Impact of Continuing CFC‐11 Emissions on Stratospheric Ozone E. Fleming et al. 10.1029/2019JD031849
- On the link between atmospheric cloud parameters and cosmic rays J. Christodoulakis et al. 10.1016/j.jastp.2019.04.012
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- WACCM-D-Whole Atmosphere Community Climate Model with D-region ion chemistry P. Verronen et al. 10.1002/2015MS000592
- The influence of Middle Range Energy Electrons on atmospheric chemistry and regional climate P. Arsenovic et al. 10.1016/j.jastp.2016.04.008
18 citations as recorded by crossref.
- Implications of potential future grand solar minimum for ozone layer and climate P. Arsenovic et al. 10.5194/acp-18-3469-2018
- Direct visualization of radiation-induced transformations at alkali halide–air interfaces S. Riechers et al. 10.1038/s42004-021-00486-2
- Middle atmospheric ozone, nitrogen dioxide and nitrogen trioxide in 2002–2011: SD-WACCM simulations compared to GOMOS observations E. Kyrölä et al. 10.5194/acp-18-5001-2018
- On the discrepancy of HCl processing in the core of the wintertime polar vortices J. Grooß et al. 10.5194/acp-18-8647-2018
- Evaluation of CESM1 (WACCM) free-running and specified dynamics atmospheric composition simulations using global multispecies satellite data records L. Froidevaux et al. 10.5194/acp-19-4783-2019
- Hemispherical Asymmetry of the Lower Stratospheric O3 Response to Galactic Cosmic Rays Forcing N. Kilifarska 10.1021/acsearthspacechem.6b00009
- Cosmic Noise Absorption During Solar Proton Events in WACCM‐D and Riometer Observations E. Heino et al. 10.1029/2018JA026192
- TERRESTRIAL EFFECTS OF NEARBY SUPERNOVAE IN THE EARLY PLEISTOCENE B. Thomas et al. 10.3847/2041-8205/826/1/L3
- Simulated seasonal impact on middle atmospheric ozone from high-energy electron precipitation related to pulsating aurorae P. Verronen et al. 10.5194/angeo-39-883-2021
- Solar forcing for CMIP6 (v3.2) K. Matthes et al. 10.5194/gmd-10-2247-2017
- Effect of Precipitating Energetic Particles on the Ozone Layer and Climate E. Rozanov 10.1134/S1990793118040152
- Quasi-Decadal Variations of Lower Stratosphere Meteorological Parameters and Total Ozone Global Fields Based on Satellite Data K. Visheratin & M. Kalashnik 10.1134/S0001433818090414
- The Impact of Continuing CFC‐11 Emissions on Stratospheric Ozone E. Fleming et al. 10.1029/2019JD031849
- On the link between atmospheric cloud parameters and cosmic rays J. Christodoulakis et al. 10.1016/j.jastp.2019.04.012
- Magnetic-local-time dependency of radiation belt electron precipitation: impact on ozone in the polar middle atmosphere P. Verronen et al. 10.5194/angeo-38-833-2020
- Integrated atomic force microscopy and x-ray irradiation for in situ characterization of radiation-induced processes S. Riechers et al. 10.1063/5.0054646
- From Cosmic Explosions to Terrestrial Fires? A Discussion F. Deschamps & F. Mottez 10.1086/709750
- Chemical Composition of Gas-Phase Positive Ions during Laboratory Simulations of Titan’s Haze Formation J. Berry et al. 10.1021/acsearthspacechem.8b00139
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Short summary
Two global models were used to investigate the impact of galactic cosmic ray (GCRs) on the atmosphere over the 1960-2010 time period. The primary impact of the naturally occurring GCRs on ozone was found to be due to their production of NOx and this impact varies with the atmospheric chlorine loading, sulfate aerosol loading, and solar cycle variation. GCR-caused decreases of annual average global total ozone were computed to be 0.2 % or less.
Two global models were used to investigate the impact of galactic cosmic ray (GCRs) on the...
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