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First 327 results for ” R Buras”

1. 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

   Publication

2. The effect of updating scavenging and conversion rates on cloud droplets and ice particles in the TM global chemistry transport model

   In this technical report we document the updates which have been made to the heterogeneous reacti...

   JE Williams, GJ van Zadelhoff, MP Scheele | Year: 2009 | Pages: 45

   Publication

3. Comparison of south-east Atlantic aerosol direct radiative effect over clouds from SCIAMACHY, POLDER and OMI–MODIS

   The direct radiative effect (DRE) of aerosols above clouds has been found to be significant over ...

   M. de Graaf, R. Schulte, F. Peers, F. Waquet, L.G. Tilstra, P. Stammes | Journal: Atmospheric Chemistry and Physics | Volume: 20 | Year: 2020 | doi: https://doi.org/10.5194/acp-20-6707-2020

   Publication

4. Evaluating the diurnal cycle of South Atlantic stratocumulus clouds as observed by MSG SEVIRI

   Marine stratocumulus (Sc) clouds play an essential role in the earth radiation budget. Here, we c...

   Seethala, C., Meirink, J. F., Horv´ath, A., Bennartz, R., and Roebeling, R | Journal: Atmospheric Chemistry and Physics | Volume: 18 | Year: 2018 | doi: https://doi.org/10.5194/acp-18-13283-2018

   Publication

5. Global NOx emission estimates derived from an assimilation of OMI tropospheric NO2 columns

   A data assimilation system has been developed to estimate global nitrogen oxides (NOx) emissions ...

   K Miyazaki, H Eskes, K Sudo | Status: submitted | Journal: Atm. Chem. Phys. | Year: 2011 | doi: doi:10.5194/acpd-11-31523-2011

   Publication