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Improved Use of Scatterometer Measurements by Using Stress-Equivalent Reference Winds
Numerical weather prediction (NWP) and buoy ocean surface winds show some systematic differences ...
J de Kloe, ACM Stoffelen, AH Verhoef | Status: published | Journal: IEEE Journal of Selected Topics in Applied Earth O | Volume: 10 | Year: 2017 | First page: 2340 | Last page: 2347 | doi: 10.1109/JSTARS.2017.2685242
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Definition of Basic Polar Data Product
During the OPERA project an additional deliverable for working group 1 has been identified. This ...
I Holleman, G Galli | Year: 2003
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KNMI contribution to the WMO Laboratory Intercomparison of Rainfall Intensity Gauges
The Commission for Instruments and Methods of Observation (CIMO-XII Casablanca, 1998) of the Worl...
W. Wauben | Year: 2006 | Pages: 174
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Internal variability of the wind-driven ocean circulation
The ocean circulation is known to vary on a multitude of time and spatial scales.
Due to the larg...
CA Katsman | University: Utrecht | Year: 2001
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Bifurcations in a low-order model with self-interaction
For finite the equivalent depth, the shallow-water equations (SWE) exhibit instabilities based on...
RJ Haarsma, JD Opsteegh | Status: published | Journal: Tellus | Volume: 43A | Year: 1991 | First page: 266 | Last page: 276
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