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First 930 results for ” T Roeckmann”

1. The impact of precipitation evaporation on the atmospheric aerosol distribution in EC-Earth v3.2.0

   The representation of aerosol–cloud interaction in global climate models (GCMs) remains a large s...

   M de Bruine, M Krol, T van Noije, P Le Sager, T Röckmann | Status: published | Journal: Geosci. Model Dev. | Volume: 11 | Year: 2018 | First page: 1443 | Last page: 1465 | doi: 10.5194/gmd-11-1443-2018

   Publication

2. COST-716 Near Real-Time Demonstration Project, International Works
   H van der Marel, E Brockmann, S de Haan, J Dousa, J Johansson | Conference: GPS Meteorology: Ground-Based and Space-Borne Applications | Organisation: JMA | Place: Tsukuba | Year: 2003 | First page: 0 | Last page: 0

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3. 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

4. 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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5. 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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