Liste complète des notices publiques
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- Point sur les travaux de l'e-Navigation et de la modernisation du SMDSM
- Modéliser & simuler : épistémologies et pratiques de la modélisation et de la simulation. Tome 1, vol. 2
- Basis for a Rainfall Estimation Technique Using IR-VIS Cloud Classification and Parameters over the Life Cycle of Mesoscale Convective Systems
- D09109 - Factors controlling the interannual variability in the carbon balance of a southern boreal black spruce forest (DOI 10.1029/2007JD008965)
- Composition and Chemistry - D20305 - Characterization of the atmospheric temperature and moisture conditions above Dome C (Antarctica) during austral summer and fall months (DOI 10.1029/2005JD006976)
- Measurement of effect of chemical reactions on the hydrologic properties of fractured glass media using a tri-axial flow and transport apparatus
- 45 BEACON - TELEVISION SEATS OF APPROVAL
- Statistical Characteristics of Prognostic Meteorological Fields and Their Use in Objective Analysis
- Propagations and reflections of long equatorial waves in the tropical pacific ocean during the 1986-1989 and 1992-1993ENSO events as observed from geosat, TOPEX/Poseidon and TOGA-TAO data
- Impact of satellite cloud motion winds on HIRLAM forecasts.
- Microburst observations in tropical Australia
- Investigation of systematic errors by relaxation experiments
- Volatility of aerosol at Mace Head, on the west coast of Ireland
- A note on smoke concentration prediction in Athens, Greece
- INFORMATIONS CONCERNANT L ENVIRONNEMENT ET NAVIGATION MARITIME AU XXIEME SIECLE
- SISTEMA PROGRAMM PERVICHNOJ OBRABOTKI NA FORTRANE
- APPLICATION OF A CLOUD MODEL TO COOLING TOWER PLUMES AND CLOUDS
- THE RELATIONSHIP BETWEEN THE GRADIENT OF SATELLITE-DERIVED RADIANCE AND UPPER TROPOSPHERIC / LOWER STRATOSPHERIC WINDS
- A ATMOSPHERIC SECTION - Hail Detection Using S- and C-Band Radar Reflectivity Difference
- CLIMATE INFORMATION AND PREDICTION SERVICES (CLIPS) FOCAL POINT TRAINING WORKSHOP FOR REGIONAL ASSOCIATION III. Lima, Peru, 8-19 August 2005; WMO/TD N°1293.