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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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Observation of Hydrological Processes Using Remote Sensing
The availability of spatial information on water quantity and quality enables closure of the wat...
B Su, RA Roebeling, I Holleman et al. | Year: 2011
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Analysis of seasonal ocean bottom pressure variability in the Gulf of Thailand from GRACE
Since its launch in 2002, the Gravity Recovery and Climate Experiment (GRACE) has proven to be an...
B Wouters, D Chambers | Status: published | Journal: Glob. Plan. Change | Volume: 74 | Year: 2010 | First page: 76 | Last page: 81 | doi: 10.1016/j.gloplacha.2010.08.002
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Earthquake Data in Engineering Seismology: Predictive Models, Data Management and Networks (
This book addresses current activities in strong-motion networks around the globe, covering issue...
S Akkar, P Gülkan, T van Eck | Year: 2011 | Publisher: Springer
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How much could be gained from ocean-data assimilation if ENSO were a simple stochastic oscillator?
Assimilation of sub-surface ocean data is one of the factors that have contributed to the increas...
G Burgers | Conference: Third WMO international symposium on assimilation | Organisation: WMO (Geneva 2000) | Place: Quebec City | First page: 0 | Last page: 0
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