Liste complète des notices publiques
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- Le climat : de l'observation à la modélisation : brève histoire d'une épopée scientifique et technologique / par Ludovic Touzé-Peiffer [Note de lecture]
- Cours de météorologie adapte à la préparation des Licences de Pilote Professionnel d'avion et de qualification de vol aux instruments. Fascicule IV
- Recherches concernant un hygromètre
- Das Klima von Calw nach hundertjährigen Wetterbeobachtungen
- D17311 - Characterizing the transport pathways of Asian dust (DOI 10.1029/2007JD009674)
- Composition and Chemistry - D04303 - Atmospheric transport of elemental carbon (DOI 10.1029/2005JD006505)
- A Feasibility Study for Simultaneous Estimates of Water Vapor and Precipitation Parameters Using a Three-Frequency Radar
- Climate and Dynamics - D19104 - All-sky imaging observations of inesospheric fronts in 01557.7 nm and broadband OH airglow emissions: Analysis of frontal structure, atmospheric background conditions, and potential sourcing mechanisms (
- Flow fluid characteristics and their relationship to the intensity of drifting sand activity in the Taklimakan desert
- Annual review of the world climate research programme and report of session of the joint scientific committee.
- Climate information for the application of solar energy
- Factors wich affected movement of tropical cyclone connie in AMEX phase 2
- Issledovanie izmenchivosti vysoty nizhnej granitsy oblakov
- Computer modelling of the global behaviour of the atmosphere ocean system and its sensitivity to the anthropogenic effects
- The auroral ionosphere and thermosphere
- AN INVESTIGATION OF THE ENVIRONMENTAL IMPACT OF AN ARTIFICIAL THERMAL PLUME
- BUOYANCY AND PRESSURE PERTURBATIONS DERIVED FROM DUAL-DOPPLER RADAR OBSERVATIONS OF THE PLANETARY BOUNDARY LAYER : APPLICATIONS FOR MATCHING MODELS WITH OBSERVATIONS
- ENERGY BUDGET OF THE EQUATORIAL ATMOSPHERE AND MERIDIONAL HEAT TRANSFER
- CURRENT METHODS FOR THE STUDY OF EVAPORATION FROM WATER SURFACES AND EVAPOTRANSPIRATION
- ESTIMATION DE LA DIFFUSIVITE TURBULENTE SUIVANT LA VERTICALE EN PARTANT DES PROFILS DU THORON