Liste complète des notices publiques
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- Sentinel-6, vers une quatrième décennie d'observation du niveau des océans
- Tropical Cyclones and Climate Change Assessment: Part I: Detection and Attribution
- Précis général des nuisances : nuisances dues aux activités urbaines
- Quantum d'actions et nombres transcendants
- Seasonal variation of PM10-bound PAHs in the atmosphere of Xiamen, China
- Upscale effects in simulations of tropical convection on an equatorial beta-plane
- Composition and Chemistry - ACH 2. Controls on the emission of plant volatiles through stomata: Differential sensitivity of emission rates to stomatal closure explained (DOI 10.1029/2002JD002620)
- Composition and Chemistry (ACH) - ACH 1 - Ozone profile differences between Europe and New Zealand: Effects on surface UV irradiance and its estimation from satellite sensors (DOI 10.1029/2002JD002770)
- Special Section: SAGE III-Ozone Loss and Validation Experiment and Third European Stratospheric Experiment on Ozone-2000 (SOLVE/THESEO), Part 2: SOL 52 Global tracer modeling during SOLVE: High-latitude descent and mixing
- Cooling of the Arctic and Antarctic polar stratospheres due to ozone depletion
- Vertical diffusion parameter in the atmospheric boundary layer
- Seventh conference on probability and statistics atmospheric sciences 2-6 november 1981, monterey, Calif
- INFLUENCE DES SYSTEMES DEPRESSIONNAIRES SUR L EVALUATION DE LA THERMOCLINE SAISONNIERE
- OB EKTIVNYJ ANALIZ TEMPERATURY POVERKHNOSTNOGO SLOYA OKEANA V SEVERO-VOSTOCHNOJ ATLANTIKE
- KLIMATSKI OPIS IN OCENA VPLIVA OJEZERITVE CERKNISKEGA IN PLANINSKEGA POLJA NA SPREMEMBO MIKROKLIME
- FLUKTUATSII TEMPERATURY I VODNOSTI V ZONE PROSVETLENIYA OBLACHNOJ SREDY
- RATE OF ENERGY TRANSFER FROM INTERNAL WAVES TO THE MAIN FLOW IN THE UPPER ATMOSPHERE
- Surface water characteristics in NCEP global spectral model and reanalysis
- Influence des surfaces continentales sur la variabilité du cycle hydrologique des échelles inter-annuelle à multi-décennale : une brève histoire de la " dérive des continents " dans les modèles de climat
- Pourquoi les rivières débordent-elles ?