Liste complète des notices publiques
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- Des modèles climatiques plus robustes
- Vient de paraître [La Météorologie n°118]
- Guide des qualifications et de la formation du personnel météorologique employé à la protection météorologique de la navigation aérienne internationale
- Optical observations of chemical releases in the upper atmosphere during 1969, with description of instrument used for day time vaportrail tracking
- Mémoires de l'Académie royale des sciences depuis 1666 jusqu'en 1699. Tome V
- Impact of the Saharan dust outbreaks on the ambient levels of total suspended particles (TSP) in the marine boundary layer (MBL) of the Subtropical Eastern North Atlantic Ocean
- The Influence of the Solar Cycle and QBO on the Late-Winter Stratospheric Polar Vortex
- Interrelation between the vegetation index and the climatic parameters and structural characteristics of vegetation cover
- Global tracer transport models. Report of a scientific symposium (the Bermuda biological station for research, Bermuda, 10-13 december 1990).
- Aerosol and Clouds - D22206 - Mapping annual mean ground-level PM25 concentrations using Multiangle Imaging Spectroradiometer aerosol optical thickness over the contiguous United States (DOI 10.1029/2004JD005025)
- Atmospheric nitric acid concentrations in a mediterranean site, Patras, Greece
- A scatterometry research programme
- Decreasing diurnal temperature range : CO2 greenhouse or SO2 energy balance effect ?
- Symposium on global climatic effects of aerosols, 11-13 October 1989, held at the eighth annual meeting of the American Association for aerosol research, Reno-Sparks, Nevada, 9-13 October 1989
- SIMPLE STATISTICAL MODEL OF THE PRESENT-DAY CLIMATE
- GRAPHE CLIMATIQUE
- THE RESURGENCE OF AGRICULTURAL METEOROLOGY
- Variation and long-term trends in tropospheric methane [CH4] concentration over Japan Since 1986
- Die Beobachtungen der horizontal-intensität des erdmagnetismus im observatorium zu katharinenburg von 1841-1889
- NOTE SUR L'ABAQUE POUR LA DETERMINATION DU VENT DU GRADIENT D'APRES L'ECARTEMENT DES ISOHYPSES D'UNE MEME SURFACE ISOBARE