Liste complète des notices publiques
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- Dramatic sea-ice melt caps tough Arctic summer
- Defining a New Normal for Extremes in a Warming World
- Assemblée générale de Vannes, 22-23 septembre 1934 et rapports sur les ressources immenses des climats de Bretagne, 3 février 1935 : compte-rendu, voeux et décisions
- Assessing Bias and Uncertainty in the HadAT-Adjusted Radiosonde Climate Record
- Impact of Anomalous Ocean Heat Transport on the North Atlantic Oscillation
- Climate and Dynamics - D13104 - Kelvin wave signatures in ECMWF meteo fields and Global Ozone Monitoring Experiment (GOME) ozone columns (DOI 10.1029/2004JD005261)
- Modeling wind-blown desert dust in the southwestern United States for public health warning: A case study
- A ATMOSPHERIC SECTION - Atmospheric Emitted Radiance Interferometer. Part I: Instrument Design
- C08010 - Roles of vertical correlations of background error and T-S relations in estimation of temperature and salinity profiles from sea surface dynamic height (DOI 10.1029/2003JC002224)
- Special Section: Layered Phenomena in the Mesopause Region (LPMR) - PMR 12 - Solar backscattered ultraviolet (SBUV) observations of polar mesospheric clouds (PMCS) over two solar cycles (DOI 10.1029/2002JD002398)
- Variations in leaf temperature, plant internal resistance, photon requirement and transpiration of pigeonpea under bare and mulched soil conditions
- Nonlinear energy exchanges among super cloud clusters, cloud clusters and intraseaonal variations
- Model estimates of turbulence characteristics of cumulonimbus hail and storm cloud for analysis of their state and degree of development
- CONTRIBUTION A L ETUDE DE LA STRUCTURE TURBULENTE DE LA COUCHE LIMITE CONVECTIVE SAHELIENNE EN PRESENCE DE BRUME SECHE
- AZ ULTRAVIOLA NAPSUGARZAS ES HATASAI
- THE ASSOCIATION BETWEEN LATITUDINAL TEMPERATURE GRADIENT AND EDDY TRANSPORT. PART 2 : RELATIONSHIPS BETWEEN SENSIBLE HEAT TRANSPORT BY STATIONARY WAVES AND WIND, PRESSURE AND TEMPERATURE IN WINTER
- UN MODELE ANALYTIQUE D ADVECTION LOCALE
- TEMPERATURE AND HUMIDITY STRUCTURE OF THE SUB-CLOUD LAYER OVER LAND
- Further analysis of semidiurnal tidal motions between 30 and 60 kilometers
- Pyranomètre CE180