Articles | Volume 16, issue 1
https://doi.org/10.5194/acp-16-195-2016
© Author(s) 2016. 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-16-195-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Can we explain the observed methane variability after the Mount Pinatubo eruption?
Meteorology and Air Quality, Wageningen University and Research Center, Wageningen, The Netherlands
Netherlands Institute for Space Research (SRON), Utrecht, The Netherlands
Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Utrecht, The Netherlands
M. van Weele
Royal Netherlands Meteorological Institute (KNMI), De Bilt, The Netherlands
T. van Noije
Royal Netherlands Meteorological Institute (KNMI), De Bilt, The Netherlands
P. Le Sager
Royal Netherlands Meteorological Institute (KNMI), De Bilt, The Netherlands
T. Röckmann
Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Utrecht, The Netherlands
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Cited
10 citations as recorded by crossref.
- Constraints and biases in a tropospheric two-box model of OH S. Naus et al. 10.5194/acp-19-407-2019
- Investigation of the global methane budget over 1980–2017 using GFDL-AM4.1 J. He et al. 10.5194/acp-20-805-2020
- Methane Feedbacks to the Global Climate System in a Warmer World J. Dean et al. 10.1002/2017RG000559
- Using machine learning to construct TOMCAT model and occultation measurement-based stratospheric methane (TCOM-CH4) and nitrous oxide (TCOM-N2O) profile data sets S. Dhomse & M. Chipperfield 10.5194/essd-15-5105-2023
- On the role of trend and variability in the hydroxyl radical (OH) in the global methane budget Y. Zhao et al. 10.5194/acp-20-13011-2020
- Variations of methane stable isotopic values from an Alpine peatland on the eastern Qinghai-Tibetan Plateau Q. Guo et al. 10.1007/s11631-021-00477-z
- Overlooked Long‐Term Atmospheric Chemical Feedbacks Alter the Impact of Solar Geoengineering: Implications for Tropospheric Oxidative Capacity J. Moch et al. 10.1029/2023AV000911
- What do we know about the global methane budget? Results from four decades of atmospheric CH4observations and the way forward X. Lan et al. 10.1098/rsta.2020.0440
- C-IFS-CB05-BASCOE: stratospheric chemistry in the Integrated Forecasting System of ECMWF V. Huijnen et al. 10.5194/gmd-9-3071-2016
- Emissions from the Oil and Gas Sectors, Coal Mining and Ruminant Farming Drive Methane Growth over the Past Three Decades N. CHANDRA et al. 10.2151/jmsj.2021-015
10 citations as recorded by crossref.
- Constraints and biases in a tropospheric two-box model of OH S. Naus et al. 10.5194/acp-19-407-2019
- Investigation of the global methane budget over 1980–2017 using GFDL-AM4.1 J. He et al. 10.5194/acp-20-805-2020
- Methane Feedbacks to the Global Climate System in a Warmer World J. Dean et al. 10.1002/2017RG000559
- Using machine learning to construct TOMCAT model and occultation measurement-based stratospheric methane (TCOM-CH4) and nitrous oxide (TCOM-N2O) profile data sets S. Dhomse & M. Chipperfield 10.5194/essd-15-5105-2023
- On the role of trend and variability in the hydroxyl radical (OH) in the global methane budget Y. Zhao et al. 10.5194/acp-20-13011-2020
- Variations of methane stable isotopic values from an Alpine peatland on the eastern Qinghai-Tibetan Plateau Q. Guo et al. 10.1007/s11631-021-00477-z
- Overlooked Long‐Term Atmospheric Chemical Feedbacks Alter the Impact of Solar Geoengineering: Implications for Tropospheric Oxidative Capacity J. Moch et al. 10.1029/2023AV000911
- What do we know about the global methane budget? Results from four decades of atmospheric CH4observations and the way forward X. Lan et al. 10.1098/rsta.2020.0440
- C-IFS-CB05-BASCOE: stratospheric chemistry in the Integrated Forecasting System of ECMWF V. Huijnen et al. 10.5194/gmd-9-3071-2016
- Emissions from the Oil and Gas Sectors, Coal Mining and Ruminant Farming Drive Methane Growth over the Past Three Decades N. CHANDRA et al. 10.2151/jmsj.2021-015
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Latest update: 02 Nov 2024
Short summary
We quantify the processes responsible for methane growth rate variability in the period 1990 to 1995, a period with variations in climate and radiation due to the Pinatubo eruption. We find significant contributions from changes in the methane emission from wetlands, and in the methane removal by OH caused by stratospheric aerosols, by the decrease in temperature and water vapour, by stratospheric ozone depletion and by changes in emissions of CO and NMVOC.
We quantify the processes responsible for methane growth rate variability in the period 1990 to...
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