Liste complète des notices publiques
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- [Résumé climatique] Décembre 1998
- Brewster's dark patch: a neglected optical phenomenon in the landscape
- La météorologie de Jupiter
- Regional estimation of base flow for the conterminous United States by hydrologic landscape regions
- Simulations of the Madden-Julian oscillation in four pairs of coupled and uncoupled global models
- Composition and Chemistry - D14305 - Comment on "Enhanced upper stratospheric ozone: Sign of recovery or solar cycle effect?" by W. Steinbrecht et al. (DOI 10.1029/2004JD004826)
- Special Section: SAGE III-Ozone Loss and Validation Experiment and Third European Stratospheric Experiment on Ozone-2000 (SOLVE/THESEO), Part 2: SOL 55 Microphysical modeling of the 1999-2000 Arctic winter: 1. Polar stratospheric clouds,denitrification clouds, and dehydratation
- Simulation of exact barotropic vorticity equation solutions using a spectral model
- Elevational changes in meteorological variables along a midlatitude glacier during summer
- Computer modeling of processes of polarized light scattering by spherical microparticles [homogeneous, hollow, two layered] in laser sounding systems
- Influence of precipitating convective on the surface energy budget observed during a tropical ocean global atmosphere pilot cruise in the tropical western Pacific ocean
- The effect of man's activities on climatic changes
- O sovmestnom uchete vliyaniya faktorov vneshnej sredy na prodolzhitel'nost' mezhfaznykh periodov rastenij
- A meteorologiai tenyezok hatasa az oszi buza level feluletenek, magassaganak es szerves anyas tartalmanak novekedesere
- PROSTRANSTVENNO-VREMENNAYA IZMENCHIVOST MERIDIONAL NOGO PERENOSA TEPLA V OKEANAKH
- OB ODNOM ASIMPTOTICHESKOM METODE RESHENIYA ZADACHI GIDRODINAMICHESKOGO KRATKOSROCHNOGO PROGNOZA POGODY
- THE DIURNAL VARIATION OF AIR TEMPERATURE
- Effects of gravel and sand mulches on dew deposition in the semiarid region of China
- The Labrador Sea Deep Convection Experiment - ARTICLES - Quasi-decadal Salinity Fluctuations in the Labrador Sea
- The frontal width problem