Liste complète des notices publiques
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- Pour un nouvel élan de la recherche polaire
- A Robust Numerical Solution of the Stochastic Collection-Breakup Equation for Warm Rain
- Summer Temperature Variations in the European Alps, A.D. 755-2004
- Five-day mean 500 hPa height and mean sea level pressure fields for the northern hemisphere (1946-1977). Volume 3 : summer.
- Effects of a dynamic ocean on simulated climate sensitivity to greenhouse gases
- Abilities and Limitations of a Radar-RASS wind profiler for the measurement of momentum flux in the planetary boundary layer
- Aerosol impact on the surface UV radiation from the ground-based measurements taken at Belsk, Poland, 1980-1996
- The Hirlam-Stat-archive and its applications programs
- Vertical profiles of N2O5, HO2NO2, and NO2 inside the Arctic vortex, retrieved from nocturnal MIPAS-B2 infrared limb emission measurements in february 1995
- The improvement of telecommunication performance by introduction of vsat technology in meteorological operations [final paper for the WMO international conference on Meteorological and hydrological technology ant it's management meohytec 21]drological applications
- A technique for analyzing optimal relationships among multiple sets of data fields. Part 2 : a reliability case study
- Sensitivity of Meiyu and its circulation system on large scale humidity fields over indian ocean-bay of Bengal and western Pacific-south China sea
- KVAZIPERIODICHESKIE FLUKTUATSII ATMOSFERNOGO DAVLENIYA S PERIODAMI 20-180 MIN.
- AUTOMATED ANALYSIS OF THE PRECIPITATIONS SAMPLED IN THE BACKGROUND POLLUTION AND PRECIPITATION QUALITY SURVEILLANCE NETWORK, SECTION IV
- A COMPARISON OF CONCENTRATIONS OF FISSION PRODUCTS, RADON 222, AND CLOUD CONDENSATION NUCLEI OVER THE NORTH ATLANTIC
- GRID TURBULENCE IN AIR AND WATER
- A LAGRANGIAN MODEL OF THE LOS ANGELES SMOG AEROSOL
- NYAKOM OSNOVNI PROBLEMI NA STRATOSFERNO-MEZOSFERNITE VZAIMNI VRUZKI I VLIYANIYA
- DIURNAL VARIATION OF WIND AND TEMPERATURE FIELDS IN THE EKMAN LAYER
- Lagrangian stochastic modeling of a fluctuating plume in the convective boundary layer