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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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The effect of reported high-velocity small raindrops on inferred drop size distributions and derived power laws
It has recently been shown that at high rainfall intensities, small raindrops may fall with much ...
H Leijnse, R Uijlenhoet | Status: published | Journal: Atm. Chem. Phys. | Volume: 10 | Year: 2010 | First page: 6807 | Last page: 6818 | doi: 10.5194/acp-10-6807-2010
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The “Normality” of El Niño
The amplitude of the El Niño-Southern Oscillation (ENSO) would be normally distributed if the cou...
G Burgers, DB Stephenson | Status: published | Journal: Geophys. Res. Lett. | Volume: 26 | Year: 1999 | First page: 1027 | Last page: 1030
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Shifts of means are not a proxy for changes in extreme winter temperatures in climate projections
Changes in severity of extreme weather events under influence of the enhanced greenhouse effect c...
M Schaeffer, FM Selten, JD Opsteegh | Status: published | Journal: Clim. Dyn. | Volume: 25 | Year: 2005 | First page: 51 | Last page: 63 | doi: 10.1007/s00382-004-0495-9
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Detection of the trend and seasonal variation in tropospheric NO2 over China
The results of a trend study on the tropospheric NO2 column over China are presented, on the basi...
RJ van der A, DHMU Peters, HJ Eskes, KF Boersma, M Van Roozendael, I De Smedt, HM Kelder | Status: published | Journal: J. Geophys. Res. | Volume: 111 | Year: 2006 | doi: 10.1029/2005JD006594
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