Liste complète des notices publiques
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- La climatologie [7eme édition]
- Decoupling between Precipitation Processes and Mountain Wave Induced Circulations Observed with a Vertically Pointing K-Band Doppler Radar
- Charcot et son oeuvre : La carrière du "Pourquoi Pas ?"
- Bulletin annuel de la Commission de météorologie du département de l'Yonne [Année 1926]
- New version of the TOMCAT/SLIMCAT off-line chemical transport model: Intercomparison of stratospheric tracer experiments
- Evidence that nitric acid increases relative humidity in low-temperature cirrus clouds
- Climate and Dynamics (ACL) - ACL 3. Variability of snow accumulation and isotopic composition on Nevado Sajama, Bolivia (DOI 10.1029/2003JD003623)
- Special Sections: Physical and Biochemical Evolution of the Eastern Mediterranean in the '90s (PBE) - PBE 10. Continuing influence ofthe changed thermohaline circulation in the eastern Mediterranean oil the distribution of dissolved oxygen and nutrients : physical and chemical characterization of the water masses
- Internal and external variability in a baroclinic atmosphere
- Tropical Cyclogenesis via Convectively Forced Vortex Rossby Waves in a Three-Dimensional Quasigeostrophic Model
- UV Change and QBO Effects and Major Stratosphere Warmings in the GISS Middle Atmosphere Model
- Ein messnetz fuer umweltmeteorologische untersuchungen im Salzburger zentralraum
- Comparison over France ot two methods of monthly rainfalls assessment
- CALCULATIONS OF THE FLUXES OF THERMAL RADIATION BY SPECTRAL AND INTEGRAL METHODS
- THE BEAUFORT SCALE [ REVISED 1906 ]
- INTERNATIONAL CONFERENCE ON CLIMATE AND OFFSHORE ENERGY RESOURCES, 21-23 OCTOBER 1980, LONDON, ENGLAND
- PARAMETERIZATION OF THE VERTICAL FLUX OF LATENT HEAT AT THE EARTH S SURFACE FOR USE IN STATISTICAL-DYNAMICAL CLIMATE MODELS
- AN OBSERVATIONAL STUDY OF THE STRUCTURE OF THE NOCTURNAL BOUNDARY LAYER
- MARINE STRATOCUMULUS CONVECTION. 1. GOVERNING EQUATIONS AND HORIZONTALLY HOMOGENEOUS SOLUTIONS. 2. HORIZONTALLY INHOMOGENEOUS SOLUTIONS
- A One-dimensional Time Dependent Cloud Model