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On the role of convection and turbulence for tropospheric ozone and its precursors
Ozon (O3) is een belangrijk sporengas in de troposfeer : het is een broeikasgas, het is giftig vo...
DJL Olivie | University: Eindhoven | Year: 2005
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Guidance on the use of meteorological time series constructed to match the KNMI’23 climate scenarios
In the previously issued KNMI climate scenarios Klein Tank et al. (2014), time-series of weather ...
H.W. van den Brink, C.F. de Valk | Year: 2023 | Pages: 35
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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
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Fate of the Equatorial Undercurrent in the Atlantic
The fate of water masses in the Equatorial Undercurrent (EUC) in the Atlantic is studied in a hig...
W Hazeleger, P de Vries | Year: 2003
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Arctic winter: comparison of nudged GCM runs with observations
We have compared satellite and balloon observations of methane (CH4) and hydrogen fluoride (HF) d...
M Aalst, A Bregman, C Brühl, B Steil, G Toon, S Garcelon, G Hansford, R Jones, T Gardiner, G Roelofs, J Lelieveld, P Crutzen | Status: published | Journal: Atm. Chem. Phys. | Volume: 4 | Year: 2004 | First page: 81 | Last page: 93 | doi: http://www.cosis.net/members/journals/df/abstract.php?a_id=498
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