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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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El Niño blijft El Niño
De komende eeuw zal de wereld door de toenemende concentratie van broeikasgassen waarschijnlijk z...
SY Philip, GJ van Oldenborgh | Journal: Nederlands Tijdschift voor Natuurkunde | Volume: 72 | Year: 2006 | First page: 304 | Last page: 308
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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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Zout, zouter, zoutst - Statistiek van de externe verzilting in Midden-West Nederland
Het Rijn-Maas mondingsgebied is één van de locaties in Nederland waar zoutindringing vanuit zee...
Jules Beersma, Adri Buishand, Sacha de Goederen (RIZA), Pieter Jacobs (RIZA) | Year: 2005 | Pages: 37
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Retrieval of Aerosol Height from the Oxygen A Band with TROPOMI
The Tropospheric Monitoring Instrument (TROPOMI), to be launched in 2015, will feature a new aero...
AFJ Sanders, JF de Haan, JP Veefkind | Conference: ATMOS 2012 - Advances in Atmospheric Science and Applications | Organisation: ESA | Place: Bruges, Belgium | Year: 2012 | First page: 0 | Last page: 0
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