Liste complète des notices publiques
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- Les aspects non hydrostatiques pour Aladin, Arome et Arpège
- Mémoires composés au sujet d'une correspondance météorologique, ayant pour but de parvenir à prédire le temps beaucoup à l'avance sur un point donné de la Terre. Cinquième mémoire
- Long-term observations of increasing snow cover in the western Cairngorms
- 4. Fachtagung BIOMET (19.-20. April 1999 in München) des Fachausschusses BIOMET des DMG gemeinsam mit der Gesellschaft zur Förderung Medizin-meteorologischer Forschung e.V.
- Some Features of Atmospheric Turbidity Change over the Russian Territory in the Last Quarter of the 20th Century
- Composition and Chemistry - D10301 - North American pollution outflow and the trapping of convectively lifted pollution by upper-level anticyclone (DOI 10.1029/2004JD005039)
- Climate and Dynamics - D06117 - Observed effects of horizontal radiative surface temperature variations on the atmosphere over a midwest watershed during CASES 97 (DOI 10.1029/2004JD004542)
- Climatology of Tropical Intraseasonal Convective Anomalies: 1979-2002
- Composition and Chemistry (ACH) - ACH 4 - Atmospheric budget implications of the temporal and spatial trends in methyl bromide concentration (DOI 10.1029/2002JD002943)
- Australian offshore AWS installations
- Satellite measurement of aerosol mass over land
- Late pleistocene desiccation of lake Victoria and rapid evolution of cichlid fishes
- Report on the conference "long-lived plasma formations and poorly explored forms of natural electrical discharges in the atmosphere"
- Seasonal phase lock of temporal and spatial variations of the lower cold air in the winter northern hemisphere
- Parametrizatsiya protsessov osadkoobrazovaniya v smeshannykh i ledyanykh oblakakh v chislennykh modelyakh
- The variations of monthly mean date due to their different sources
- ANCIENT CLIMATE FROM FOSSILS
- CLIMATIC IMPACT OF EXPLOSIVE VOLCANIC ERUPTIONS
- A MODEL FOR THE SPECTRAL ALBEDO OF SNOW. 1 : PURE SNOW. 2 : SNOW CONTAINING ATMOSPHERIC AEROSOLS
- Eddy-Zonal Flow Feedback in the Northern Hemisphere Winter