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Validation of KNW atlas with scatterometer winds (Phase 3 of KNW project)
The KNW (KNMI North Sea Wind) atlas is based on the ERA-Interim reanalyses dataset which captures...
I.L. Wijnant, G.J. Marseille, A. Stoffelen, H.W. van den Brink and A. Stepek | Year: 2015 | Pages: 50
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Determination of the mixing layer height from ceilometer backscatter profiles
The mixing layer height (MLH) is a key parameter in studies of many atmospheric boundary layer pr...
MJ de Haij, H Klein Baltink, WMF Wauben | Journal: KNMI Kenniscentrum | Year: 2010
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Spatial and Temporal Propagation of Scatterometer Winds
Ocean models are generally forced by synthetic (global) NWP model wind fields. It has however bee...
D Harutyunyan, A Stoffelen | Year: 2011
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GABLS 3 SCM intercomparison and evaluation, what did we learn?
A weakly stable case is selected from the Cabauw long term archive. The case is used for an evalu...
FC Bosveld, P Baas, GJ Steeneveld, AAM Holtslag | Conference: Workshop on Diurnal cycles and the stable boundary layer, | Organisation: ECMWF | Place: Reading, UK | Year: 2011 | First page: 0 | Last page: 0
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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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