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- Cours de météorologie adapté à la préparation des principales licences du personnel navigant. Fascicule IX, 1961 [Texte imprimé] / L. Buffault ; d'après le cours de météorologie de R. Beaulieu et L. Buffault
- C08007 - Estimation of submarine groundwater discharge from bulk ground electrical conductivity measurements (DOI 10.1029/2007JC004499)
- C08015 - A numerical study of melt ponds (DOI 10.1029/2006JC003729)
- A seepage face model for the interaction of shallow water tables with the ground surface: Application of the obstacle-type method
- Composition and Chemistry (ACH) ACH 3. Analysis of ozone loss in the Arctic stratosphere during the late winter and spring of 1997 using the Chemical Species Mapping on Trajectories (CSMT) technique (DOI 10. 1029/2002JD002824)
- The Microphysical Structure of Extreme Precipitation as Inferred from Ground-Based Raindrop Spectra
- Spectral properties of internal gravity waves from thunderstorms
- Transport of Mt. Pinatubo aerosol by tropospheric synoptic-scale and stratospheric planetary-scale waves
- Wave CISK of equatorial waves and the vertical distribution of cumulus heating
- Turbulence intensities and bulk coefficients in the surface layer above the sea
- Determination of the mean wind speed and momentum diffusivity profiles above tall vegetation and forest canopies using a mass conservation assumption
- On the influence of local and north Atlmantic wind forcing on the seasonal variation of sea level on the newfoundland and labrador shelf
- IMPACTS
- THE IMPACT OF ANALYSIS DIFFERENCES ON A MEDIUM-RANGE FORECAST
- MAP ACTIVITIES. BRAZIL
- FURTHER OBSERVATIONS OF THE UPLAND CLIMATE OF PLYNLIMON, MID-WALES
- O STATISTICHESKIKH PARAMETRAKH RASPREDELENIYA POLYA VETRA NA VYSOTE NAD TERRITORIEJ RUMYNII
- A NOTE ON BAROCLINIC INSTABILITY OF A SOURCE-SINK DRIVEN FLOW
- ON THE POSSIBILITY OF DETERMINING THE VERTICAL PROFILES OF AEROSOL ATTENUATION USING SATELLITE MEASUREMENTS OF REFLECTED RADIATION IN THE 0.76 MICROMETER OXYGEN BAND
- Analysis-Error Statistics of a Quasigeostrophic Model Using Three-Dimensional Variational Assimilation