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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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Time scale interaction in low-order climate models
Over the last decades, the study of climate variability has attracted ample attention. The observ...
L van Veen | University: Universiteit Utrecht | Year: 2002
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Validation of SeaWinds 25 km winds
This report is written to establish the quality of the EUMETSAT Ocean and Sea Ice Satellite Appli...
A Verhoef, J Vogelzang, A Stoffelen | Year: 2008
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Rainfall nowcasting using commercial microwave links
Accurate and timely precipitation forecasts are crucial for early warning. Rainfall nowcasting, t...
RO Imhoff, A Overeem, CC Brauer, H Leijnse, AH Weerts, R Uijlenhoet | Status: published | Journal: Geophys. Res. Lett. | Volume: 47 | Year: 2020 | doi: 10.1029/2020GL089365
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