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First 4393 results for ”W.A.A. Monna and J.J.M. den Braber”

1. The CAMS reanalysis of atmospheric composition

   The Copernicus Atmosphere Monitoring Service (CAMS) reanalysis is the latest global reanalysis da...

   A Inness, M Ades, A Agusti-Panareda, J Barré, A Benedictow, AM Blechschmidt, JJ Dominguez, R Engelen, H Eskes, J Flemming, V Huijnen, L Jones, Z Kipling, S Massart, M Parrington | Status: published | Journal: Atm. Chem. Phys. | Volume: 19 | Year: 2019 | First page: 3515 | Last page: 3556 | doi: https://doi.org/10.5194/acp-19-3515-2019

   Publication

2. Studying aerosol indirect effects by combining CM-SAF cloud microphysical property data with NO2 retrievals

   In this study the correlation between OMI tropospheric NO2 and cloud physical parameters was inve...

   R Dirksen, JF Meirink | Year: 2012

   Publication

3. A dual mass flux framework for boundary layer convection. Part II: Clouds

   This paper presents the extension of the eddy diffusivity mass flux (EDMF) framework for turbulen...

   RAJ Neggers | Status: published | Journal: J. Atmos. Sci. | Volume: 66 | Year: 2009 | First page: 1489 | Last page: 1506 | doi: 10.1175/2008JAS2636.1

   Publication

4. Chemical ozone loss in the tropopause region on subvisible ice clouds, calculated with a chemistry-transport model

   A global chemistry-transport model has been used to investigate the role of subvisible ice clouds...

   B Bregman, PH Wang, J Lelieveld | Status: published | Journal: J. Geophys. Res. | Year: 2002 | First page: 4032 | doi: 10.1029/2001JD000761

   Publication

5. Probabilistic moment tensor inversion for hydrocarbon-induced seismicity in the groningen gas field, the netherlands, part 2: Application

   Recent developments in the densification of the seismic network covering the Groningen gas field ...

   B Dost, A Stiphout, D Kuehn, M Kortekaas, E Ruigrok, S Heimann | Status: published | Journal: Bulletin of the Seismological Society of America | Volume: 110 | Year: 2020 | First page: 2112 | Last page: 2123 | doi: 10.1785/0120200076

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