Liste complète des notices publiques
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- Le guide d'un numérique plus responsable
- Elements of hamiltonian mechanics. Second edition
- Morphologie de la Tunisie présaharienne
- [Résumé climatique] Août 2012
- Understanding advances in the simulation of interseasonal variability in the ECMWF model Part I: the representation of the MJO
- Corrections - The following article is part of the special section Validation of Atmospheric Infrared Sounder Observations, which printed 16 May 2006. - D01S90 - A comparison of radiative transfer models for simulating Atmospheric Infr
- Sources and concentrations of volatile organic compounds in urban air.
- Two climatic states and feedbacks on thermohaline circulation in an Earth system model of intermediate complexity
- On the three-dimensional oceanic density distribution in a millennium integration with an AO-GCM
- Prediction experiments of hurricane Gloria [1985] using a multiply nested movable mesh model
- A new parameter scheme for radar contours of hail cells
- The exchange of fluid mass between quasi-geostrophic and ageostrophic motions during the reflection of Rossby waves from a coast. 1. the case of an infinite rectilinear coast
- SIMULATION OF THE DISTRIBUTION OF CLIMATIC ELEMENTS IN MOUNTAINOUS AREAS
- AN AIRBORNE LASER AIR MOTION SENSING SYSTEM. PART 1 : CONCEPT AND PRELIMINARY EXPERIMENT
- NEW RESULTS REGARDING THE INFLUENCE OF SOLAR ACTIVITY ON THE STRATOSPHERIC-TROPOSPHERIC EXCHANGE
- METEOROLOGISCHE PROZESSE IN DER GRUNDSCHICHT UEBER DER ANTARKTIS
- AN ANALYSIS OF SATELLITE INFRARED SOUNDINGS AT THE MESOSCALE USING STATISTICAL STRUCTURE AND CORRELATION FUNCTIONS
- Special Section: SAGE III-Ozone Loss and Validation Experiment and Third European Stratospheric Experiment on Ozone-2000 (SOLVE/THESEO) - SOL 17 Redistribution of reactive nitrogen in the Arctic lower stratosphere in the 1999/2000 winter
- How ocean vertical mixing and accumulation of warm surface water influence the "sharpness" of the equatorial thermocline
- Comparison of the last interglacial climate simulated by a coupled global model of intermediate complexity and an AOGCM