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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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On the upgrading of the modified Carbon Bond Mechanism IV for use in global Chemistry Transport Models
The modified Carbon Bond Mechanism 4 (Houweling et al., 1998) has been updated to include the mos...
JE Williams, TPC van Noije | Year: 2008 | Pages: 64
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Radiative cooling in the nocturnal boundary layer
In this thesis the transfer of infrared radiation (electromagnetic waves with a wavelength betwee...
S.A. Tjemkes | Year: 1988 | Pages: 107
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Climatological time series for the KfC project High-Quality Climate Projections (Theme 6 WP3)
After the publication of the KNMI’06 climate change scenarios for the Netherlands (Van den Hurk e...
A. Bakker | Year: 2015 | Pages: 18
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Evaluation of a new trigger function for cumulus convection
Cumulus convection plays a major role in the vertical transport of heat, moisture, momentum and c...
MJ de Haij | Year: 2005 | Pages: 117
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