Liste complète des notices publiques
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- Estimating the Transient Climate Response from Observed Warming
- Vient de paraître [La Météorologie n°55]
- Tritium profiles of pore water in the Chinese loess unsaturated zone: Implications for estimation of groundwater recharge
- Notes and Correspondence - Comments on 'Flux-gradient relationship, self-correlation and intermittency in the stable boundary layer' by C. L. Klipp and L. Mahrt (July B 2004, 130, 2087-2103)
- NOTES AND CORRESPONDENCE - The Combined Effects of Gulf Stream-Induced Baroclinicity and Upper-Level Vorticity on U.S. East Coast Extratropical Cyclogenesis
- Special Section: Particulate Matter Supersites - D07S06 - Highly time-resolved organic and elemental carbon measurements at the Baltimore Supersite in 2002 (DOI 10.1029/2004JD004610)
- The macroscopic entrainment processes of simulated cumulus ensemble. Part 2 : testing the entraining-plume model
- Observed directional characteristics of the wind wind stress and surface waves on the open ocean.
- Analysis and interpretation of VHF-radar data
- Design of a narrow-bandwidth lidar system for tropospheric hydroxyl measurements
- Non-linear interaction between the diurnal and semidiurnal tides : terdiurnal and diurnal secondary waves
- Quality control and filtering of satellite data
- The relationship between the establishment of the summer dry circulation systems in north China and the disposal of tide-generating force
- THE BOOKS OF NORMALS OF METEOROLOGICAL ELEMENTS FOR THE BRITISH ISLES FOR PERIODS ENDING 1915. SECTION II. WEEKLY, MONTHLY, QUATERLY AND SEASONAL NORMALS FOR DISTRICTS
- A CASE STUDY OF EXTENDED EAST COAST FRONTOGENESIS
- SVYAZ GARMONICHESKIK SOSTAVLYAYUSHCHIKH POLEJ H500 S ANOMALIEJ MESYACHNOGO KOLICHESTVA OSADKOV V TEPLOM POLUGODII NA DAL NEM VOSTOKE
- REFLEXION UND EMISSION NATUERLICHER OBERFLAECHEN
- MODELING VERTICAL AND HORIZONTAL DIFFUSIVITIES WITH THE SIGMA COORDINATE SYSTEM
- ON THE VALIDITY OF THE VAPOR-DEPOSITED THIN FILM OF BARIUM CHLORIDE FOR THE DETECTION OF SULFATE IN INDIVIDUAL ATMOSPHERIC PARTICLES
- Anisotropic turbulent diffusion for ozone transport at 520 K