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A SPONTANEOUS RAYLEIGH-BRILLOUIN SCATTERING EXPERIMENT FOR THE CHARACTERIZATION OF ATMOSPHERIC LIDAR BACKSCATTER (TN4 part 3)
The difference between the theoretical Rayleigh-Brillouin lineshape and the measured lineshape fr...
J de Kloe, A Stoffelen | Year: 2009
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Improving soil measurements for boundary layer research
The temperature profile in the soil is an important parameter to determine the surface heat excha...
HI Bloemink, J Bijma | Conference: TECO-2010 - WMO Technical Conference on Meteorological and Environmental Instruments and Methods of Observation | Organisation: WMO | Place: Helsinki, Finland | Year: 2010 | First page: 0 | Last page: 0
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Toward Scatterometer Winds Assimilation in the Mesoscale HARMONIE Model
Data assimilation (DA) experiments have been conducted with the high-resolution limited-area mode...
GJ Marseille, A Stoffelen | Status: accepted | Journal: IEEE Journal of Selected Topics in Applied Earth O | Year: 2017 | doi: 10.1109/JSTARS.2016.2640339
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Some sensitivities of a coupled ocean-atmosphere GCM
A coupled ocean-atmosphere GCM is being developed for use in seasonal forecasting. As part of the...
T Stockdale, M Latif, G Burgers, JO Wolfff | Status: published | Journal: Tellus | Volume: 46A | Year: 1994 | First page: 367 | Last page: 381 | doi: 10.1034/j.1600-0870.1994.t01-3-00004.x
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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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