Liste complète des notices publiques
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- Multiple Characteristics of Precipitation Inferred from Wind Profiler Radar Doppler Spectra
- Physical processes in clouds and cloud modeling
- Operations of the Weather Bureau [édition 1968]
- Workshop on Current problems in data assimilation 8-10 november 1982
- The Onset, Duration and Retreat of Rainfall in the Niger Delta Belt, Nigeria
- Consistency and normality of estimates of hydrological extremes derived from a model for fragmented data
- Wet deposition and related atmospheric chemistry in the São Paulo metropolis, Brazil. Part 3: Trends in precipitation chemistry during 1983-2003
- An Evolving Seasonal Forecasting System using Bayes' Theorem
- The forcing of divergent wind and transient vorticity fluxes to the stationary waves
- A parameterization for computing grid-averaged solar fluxes for inhomogeneous marine boundary layer clouds.Part 2 : validation using satellite data
- Variability of the global precipitable water with a timescale of 90-150 days
- A clear sky atmospheric model valid for the mediterranean zone
- Comment on "a model study of the formation of cloud condensation nuclei in remote marine areas" by Lin et al.
- DLUGOTRWALOSC LETNIEGO STRATOSFERYCZNEGO ANTYCYKLONU A SREDNIA MIESIECZNA TEMPERATURA POWIETRZA I MIESIECZNA SUMA OPADOW ATMOSFERYCZNYCH W POLSCE
- HAPEX-MOBILHY : A HYDROLOGIC ATMOSPHERIC EXPERIMENT FOR THE STUDY OF WATER BUDGET AND EVAPORATION FLUX AT THE CLIMATIC SCALE
- CALCULATION OF GROUND TEMPERATURE AND FLUXES BY SURFACE MODELS : A COMPARISON WITH EXPERIMENTAL DATA IN THE AFRICAN SAVANNAH
- CLIMATIC CHANGES AND OUTSTANDING SINGULARITIES IN THE LONDON AREA 1947-1980, WITH COMPARISONS AGAINST THE PERIOD 1881-1950. PART 5 : OCTOBER TO DECEMBER, AND REVIEW OF THE YEAR
- FURTHER STUDIES ON SINGLE STATION CLIMATOLOGY : [1] THE SUMMER CONFLUENCE OF SUBTROPIC AND POLAR FRONT JET, [2] THE TWO NORTHERN COLD POLES
- Wind energy production in cold climate
- Études de la dynamique du jet de basses couches et de son rôle sur la discontinuité frontale à partir de données du radar ST et du SODAR obtenues lors de l'expérience FRONTS 87