Liste complète des notices publiques
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- Charts of rainfall over the mediterranean region
- El Niño-Southern Oscillation influences on soybean yields in eastern Paraguay
- The representation of a synoptic-scale weather system in a thermodynamically adjusted version of the ECHAM4 general circulation model
- Construction d'un système d'analyse objective de données hétérogènes d'après les méthodes de l'interpolation optimale et de l'ajustement optimal (traduction d'un article de Gandin (L. S.) & Kagan (R. L.)
- The Coupled Boundary Layers and Air-Sea Transfer Experiment in Low Winds
- Aerosol and Clouds - D12202 - Aerosol size spectra and CCN activity spectra: Reconciling the lognormal, algebraic, and power laws (DOI 10.1029/2005JD006532)
- Currents in the Aleutian Basin and subarctic North Pacific near the dateline in summer 1993 10.1029/2005JC003064 02 March 2006
- Temporal Structure of the Solar Radiation Field in Cloudy Conditions: Are Retrievals of Hourly Averages from Space Possible?
- Aerosols and Clouds (AAC) - AAC 2 - Mass balance of free tropospheric aerosol at the Puy de Dôme (France) in winter (DOI 10.1029/2002JD002747)
- Some results of research on sandstorm in China
- Retrieval of microwave surface emittance over land using coincident microwave and infrared satellite measurements
- Estimated national releases to the atmosphere of chlorodifluoromethane [HCFC-22] during 1990
- Regimes in the wintertime circulation over northern extratropics. 1 : observational evidence
- MEASUREMENT OF WIND PARAMETERS AND HEAT FLUX WITH THE SENSITRON DOPPLER SODAR
- SRAVNENIE OB EKTIVNOGO I SINOPTICHESKOGO ANALIZA BARICHESKOGO POLYA V GIDROMETTSENTRE SSSR S OB EKTIVNYM ANALIZOM NMTS SSHA, NAKAPLIVAEMYM V BAZE DANNYKH GRID
- SATELLITE REMOTE SENSING IN HYDROLOGY
- CLIMA CONTINENTAL. LA MESETA CENTRAL DE ESPANA
- A RECENT INCREASE IN SUNSHINE DURATION WITHIN THE CONTIGUOUS UNITED STATES
- SYNOPTIC-SCALE STUDIES USING THE NIMBUS-6 SCANNING MICROWAVE SPECTROMETER
- ENERGIES ET ECHELLES DES MOUVEMENTS HORIZONTAUX LORS D UN < SAUT CONVECTIF > DANS LA BASSE ATMOSPHERE