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Comparison of tail models and data for extreme value analysis of high tide water levels along the Dutch coast
To assess the reliability of flood protection in the Netherlands, return values of wind speed and...
C.F de Valk, H.W. van den Brink | Year: 2023 | Pages: 72
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North Sea Wind Climatology Part 2: ERA-Interim and Harmonie model data
The national government needs high quality offshore wind climatology at and around hub height to ...
I.L. Wijnant, H.W. van den Brink and A. Stepek | Year: 2014 | Pages: 52
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Observation Representativeness Error
NWP models simulate the atmospheric state on a given model grid, thereby principally
limiting the...
GJ Marseille, A Stoffelen | Year: 2012
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Wind chill equivalente temperatuur
Bij vriezend weer voelt het op een winderige dag, met meer warmteverlies door de wind, kouder aan...
G Groen | Year: 2009
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Manually adjusting a numerical weather analysis using three-dimensional variational data-assimilation
A method is presented to manually adjust the analysis of a numerical weather forecasting model a...
WTM Verkley, PWC Vosbeek, AR Moene | Status: published | Journal: Quart. J. Royal Meteor. Soc. | Volume: 131 | Year: 2005 | First page: 1713 | Last page: 1736 | doi: 10.1256/qj.03.202
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