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2Observation 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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Coupled sea surface-atmospheric model 2. Spectrum of short wind waves
A physical model of the short wind wave spectrum in
the wavelength range from a few millimeters ...
VN Kudryavtsev, VK Makin, B Chapron | Status: published | Journal: J. Geophys. Res. | Volume: 104 | Year: 1999 | First page: 7625 | Last page: 7639
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Monitoring induced seismicity in the North of the Netherlands: status report 2010
This report presents an update on the results from monitoring induced seismicity in the North of ...
B Dost, F Goutbeek, T van Eck, D Kraaijpoel | Year: 2012 | Pages: 39
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A balanced approximation of the one-layer shallow-water equations on a sphere
A global version of the equivalent barotropic vorticity equation is derived for the one-layer sha...
WTM Verkley | Status: published | Journal: J. Atmos. Sci. | Volume: 66 | Year: 2009 | First page: 1735 | Last page: 1748 | doi: 10.1175/2008JAS2837.1
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NWP model error structure functions obtained from scatterometer winds
Wind vectors derived from scatterometer measurements
are spatially detailed as compared to global...
J Vogelzang, A Stoffelen | Status: published | Journal: IEEE Transactions on Geoscience and Remote Sensing | Volume: 50 | Year: 2011 | First page: 2525 | Last page: 2533 | doi: 10.1109/TGRS.2011.2168407
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