Liste complète des notices publiques
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- S'il pleut à la Saint-Médard, pleut-il vraiment 40 jours plus tard ?
- Projected increase in continental runoff due to plant responses to increasing carbon dioxide.
- Finite-Amplitude Baroclinic Instability of Time-Varying Abyssal Currents //
- Special Section: Toward Reducing Cloud-Climate Feedback Uncertainties in Atmospheric General Circulation Models - D15S12 - Organization of mesoscale convective systems: 2. Linear theory (DO) 10. 1029/2004JD005450)
- A phosphorus budget for Northern Ireland: inputs to inland and coastal waters
- Response of a Palmes tube at various fluctuations of concentration in ambient air
- Time-delayed response of the solar to long term solar magnetic cycle amplitude modulation as inferred by sunspot relative number and isotope data of 10Be in the greenland ice core and land air temperature varaition of the earth
- Histoire du dernier cycle climatique enregistrée dans la séquence loessique d'Achenheim [Alsace, France], à partir de la susceptibilité magnétique
- A simple lagrangian model of the mesoscale pollutant transport in the atmosphere
- Comments on "an empirical study of the economic effects of climate change on world agriculture", by S. Kane, J. Reilly and J. Tobey [Climatic change 21, 17-35]
- Seasonal effects on reproduction, infection and psychoses
- Biological production off southern California is linked to climatic change
- A model for the turbulent structure of the stratocumulus-topped atmospheric boundary layer
- INFLUENCE OF THE ANNUAL CYCLE IN MERIDIONAL TRANSPORT ON THE QUASI-BIENNIAL OSCILLATION IN TOTAL OZONE
- DISPERSII KOORDINAT CHASTITS PRIMESI V PRIZEMNOM SLOE ATMOSFERY
- HEMISPHERIC SIMULATION OF THE ASIAN SUMMER MONSOON
- VALENCE. CARTE CLIMATIQUE DETAILLEE DE LA FRANCE
- THE EFFECT OF ATMOSPHERIC AEROSOLS ON THE SPECTRAL AND ANGULAR DISTRIBUTIONS OF THERMAL RADIATION
- A MULTI-LAYER SPECTRAL MODEL AND THE SEMI-IMPLICIT METHOD
- Convectively generated internal gravity waves in the lower atmosphere of Venus, part 2 : mean wind shear and wave-mean flow interaction