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Upper Air Climatology of Amsterdam FIR, using ERA-Interim 1989-2008 Part 1
This report, part 1, presents upper-air climatology below 150 hPa (Flight level 430) for the Flig...
D Wolters, G Groen | Year: 2011 | Pages: 82
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Brief review of wind and drag transformations in WBI2017
To determine the hydraulic boundary conditions for the design of coastal defence structures, hydr...
A. Sterl | Year: 2018 | Pages: 12
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Precipitation amount and intensity measurements with the Ott Pluvio
The Royal Netherlands Meteorological Institute (KNMI) performs routine precipitation amount measu...
Wiel Wauben | Year: 2004 | Pages: 94
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On the effect of doubling of atmospheric CO2 on the stormtracks in the climate of a general circulation model
We have determined the effect of a doubling of the atmospheric CO2 content on the stormtracks in ...
P Siegmund | Year: 1990 | Pages: 12
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Antarctic Ozone Hole [in ”State of the Climate in 2020”]
[from the full abstract] Above Earth’s surface, the annual lower troposphere temperature equaled ...
A.T.J. de Laat | Journal: Bulletin of the American Meteorological Society | Volume: Volume 102: Issue 8 | Year: 2021 | First page: S475 | Last page: S1 | doi: 10.1175/2021BAMSStateoftheClimate.1
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