Liste complète des notices publiques
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- METEO et CLIMAT INFO n°74 - Septembre 2019
- Hurricane ! : coping with disaster : progress and challenges since Galveston, 1900
- Climate and Dynamics - D07111 - Enhanced net formations of nitrous oxide and methane underneath the frozen soil in Sanjiang wetland, northeastern China (DOI 10.1029/2006JD008025)
- South American Low Level Jet Experiment : SALLJEX.
- Comment on paper #8216Stream depletion predictions using pumping test data from a heterogeneous stream-aquifer system (a case study from the Great Plains, USA)#8217 by Stefan J. Kollet and Vitaly A. Zlotnik, vol. 281: 96#8211114
- QBO and QTO of the atmospheric trace element carbon monoxide during 1989#82112001: An update
- Surface winds at landfall of hurricane Andrew [1992]- a reply
- Complex singular value decomposition analysis of equatorial waves in the Pacific observed by TOPEX/Poseidon Altimeter
- Flow and dispersion over topography : a comparison between numerical and laboratory data for two-dimensional flows
- Granulométrie de l'aérosol marin
- Characteristics and performance of three low-cost super pressure balloon [Tetroon] systems.
- The impact of horizontal resolution on moist processes in the ECMWF model
- Lead 210 in surface air and soils from California : implications for the behavior of trace constituents in the planetary boundary layer
- Possible composition and climatic changes due to past intense energetic particle precipitation
- ENERGETICS OF THE MONSOON CIRCULATION OVER SOUTH ASIA : 1 - DIABATIC HEATING AND THE GENERATION OF AVAILABLE POTENTIAL ENERGY
- ON MERIDIONAL HEAT TRANSPORTS IN THE WORLD OCEAN
- FORCED SECONDARY CIRCULATIONS IN HURRICANES
- LE PUBLIC ET LA VULGARISATION SCIENTIFIQUE ET TECHNIQUE. ENQUETE SUR LES ATTITUDES ET LES COMPORTEMENTS DES FRANCAIS
- NUMERICAL SIMULATION OF COLD EASTERLY CIRCULATIONS OVER THE CANADIAN WESTERN PLAINS USING A MESOSCALE BOUNDARY-LAYER MODEL
- DEPENDENCE OF ANTENNA TEMPERATURE ON THE POLARIZATION OF EMITTED RADIATION FOR A SCANNING MICROWAVE RADIOMETER
