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Can we explain the observed methane variability after the Mount Pinatubo eruption?
The CH4 growth rate in the atmosphere showed large variations after the Pinatubo eruption in June...
N Bândă, M Krol, M van Weele, T van Noije, P Le Sager, T Röckmann | Status: published | Journal: Atmos. Chem. Phys. | Volume: 16 | Year: 2016 | First page: 195 | Last page: 214 | doi: 10.5194/acp-16-195-2016
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Global and regional climate impacts of future aerosol mitigation in an RCP6.0-like scenario in EC-Earth
Future changes in aerosol concentrations will influence the climate system over the coming decade...
C Chuwah, T van Noije, DP van Vuuren, P Le Sager, W Hazeleger | Status: published | Journal: Clim. Change | Volume: 134 | Year: 2016 | First page: 1 | Last page: 14 | doi: 10.1007/s10584-015-1525-9
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Global impacts of surface ozone changes on crop yields and land use
Exposure to surface ozone has detrimental impacts on vegetation and crop yields. In this study, w...
C Chuwah, T van Noije, DP van Vuuren, E Stehfest, W Hazeleger | Status: published | Journal: Atmos. Environ. | Volume: 106 | Year: 2015 | First page: 11 | Last page: 23 | doi: 10.1016/j.atmosenv.2015.01.062
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Sensitivity of methane to atmospheric and emission perturbations after the Pinatubo eruption
The growth rate of methane (CH4) showed fluctuations in the 1990s, with particularly large anomal...
N Bândă, M Krol, M van Weele, T van Noije, T Röckmann | Conference: ACCENT-Plus Symposium on Air Quality and Climate Change: Interactions and Feedbacks | Organisation: ACCENT-Plus | Place: Urbino, Italy | Year: 2011 | First page: 0 | Last page: 0
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Analysis of global methane changes after the 1991 Pinatubo volcanic eruption
The global methane (CH4) growth rate showed large variations after the eruption of Mount Pinatubo...
N Bândă, M Krol, M van Weele, TPC van Noije, T Röckmann | Status: published | Journal: Atmos. Chem. Phys. | Volume: 13 | Year: 2013 | First page: 2267 | Last page: 2281 | doi: 10.5194/acp-13-2267-2013
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