Liste complète des notices publiques
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- Bulletin de l'OMM - vol. 57 (2) - Adaptation à la variabilité du climat et aux changements climatiques
- Guide de l'aviation générale en France
- [Notices sur les principaux instruments de la maison Richard Frères [Partie météorologie. Fascicule : DM concernant humidité , évaporation , pluie , radiation solaire ] ]
- Evolution of a subgrid deep convection parameterisation in a limited area model with increasing resolution
- Las precipitaciones maximas en 24 horas y sus periodos de retorno en España. Un estudio por regiones. Volumen 0 : Introduccion y metodologia.
- Analytical solution of the advection-diffusion equation for a ground-level finite area source
- Relationship between temperature and the seasonal course of photosynthesis in Scots pine at northern timberline and in southern boreal zone
- Climate and Dynamics - D11104 - Reassessment of the Antarctic surface mass balance using calibrated output of a regional atmospheric climate model (DOI 10.1029/2005JD006495)
- Weather Talk: Weather, or Not
- Eddy-Zonal Flow Interactions Associated with the Southern Hemisphere Annular Mode: Results from NCEP-DOE Reanalysis and a Quasi-Linear Model
- Polarization of radiothermal radiation of thice convective clouds
- PROCEEDINGS OF THE 12TH CONFERENCE OF BALTIC OCEANOGRAPHERS, APRIL 14-17, 1980 AND OF THE 7TH MEETING OF EXPERTS ON THE WATER BALANCE OF THE BALTIC SEA, APRIL 17-19, 1980. PART 1
- THE THERMALLY COUPLED RESPONSE OF THE PLANETARY SCALE CIRCULATION TO THE GLOBAL DISTRIBUTION OF HEAT SOURCES AND SINKS
- SUR LA DETERMINATION D UN ECOULEMENT FLUIDE PAR DES OBSERVATIONS DISCRETES
- HIDRODINAMIKAI MODSZER A KARPAT-MEDENCE IDOJARASANAK FINOMFELBONTASU ELOREJELZESERE. 2
- RAINFALL MINIMUM IN PENINSULAR MALAYSIA DURING THE NORTHEAST MONSOON
- EXPERIMENTAL HAIL PROTECTION IN SLOVENIA
- A Dynamic and Spatial Scaling Approach to Advection Forecasting
- Sampling strategies for the comparison of climate model calculated and satellite observed brightness temperatures
- The role of gravity waves in slowly varying in time tropospheric motions near the Equator