Liste complète des notices publiques
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- Canadians left in the cold by dwindling weather data
- Research and operational developments related to the use of satellite data in the ECMWF assimilations system
- Laboratory study of the dynamics of a layer of turbulence excited by standing surface waves
- The Influence of ENSO on the Generation of Decadal Variability in the North Pacific
- Climate and Dynamics - D15S90 - Modeling CO2 source-sink and flux over broadleaved Koreanpine forest in Changbai Mountain using inverse Lagrangian dispersion analysis (DOI 10.1029/2005JD006493)
- B OCEANIC SECTION - Adequacy of the In Situ Observing System in the Satellite Era for Climate SST
- Real-Time Implementation of Single-Doppler Radar Analysis Methods for Tropical Cyclones: Algorithm Improvements and Use with WSR-88D Display Data
- Atmospheric Sulfur and Deep Convective Clouds in tropical Pacific:A model Study
- Considerations for Use the Barnett and Preisendorfer [1987] Algorithm for Canonical Correlation Analysis of Climate Variations
- The Sensivity to Orographically Induced Gravity Wave Drag In The Geos GCM
- Solar heating rates aftervolcanic eruption : the importance of SO2 absorption
- Long-term observations of atmospheric co2 and carbon isotopes at continental sites in Germany
- COMPUTER PROGRAMS FOR FREQUENCY DISTRIBUTION ANALYSIS IN THE ROYAL OBSERVATORY HONG-KONG
- THE USE AND INTERPRETATION OF NUMERICAL WEATHER PREDICTION MODEL OUTPUT IN IDENTIFYING SYNOPTIC-SCALE ENVIRONMENTS ASSOCIATED WITH DEVELOPMENT OF MESOSCALE CONVECTIVE SYSTEMS
- COMPENDIUM OF METEOROLOGY FOR USE BY CLASS 1 AND CLASS 2 METEOROLOGICAL PERSONNEL. VOLUME 2, PART 4: TROPICAL METEOROLOGY
- TEST OF THE OGURA-CHO MODEL ON A PREFRONTAL SQUALL LINE CASE
- IZMERENIE AEHROZOL NYKH KHARAKTERISTIK I PLOTNOSTI ATMOSFERY LAZERNYM LOKATOROM
- The Conveyor belt in the OCCAM model : tracing water masses by a lagrangian methodology.
- CLIMATE SENSITIVITY TO RADIATIVE PERTURBATIONS: PHYSICAL MECHANISMS AND THEIR VALIDATION
- Quelques données numériques sur la circulation atmosphérique à haute altitude entre 20 et 30-35 km résultant de sondages exécutés à Trappes (Seine et Oise) entre le 15 octobre 1956 et le 31 mai 1957. Partie I, Texte