Liste complète des notices publiques
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- Special Section: Intercontinental Transport and Chemical Transformation 2002 (ITCT 2K2) and Pacific Exploration of Asian Continental Emissions (PEACE) Experiments - D16SO4 - Nature of unresolved complex mixture in size-distributed emis
- Characteristics of the imaginary part and single-scattering albedo of urban aerosols in northern China
- C02010. Low-frequency waves in the Santa Barbara Channel observed by high-frequency radar (DOI 10.1029/2003JC001999)
- C01010. Circulation during winter and northerly storm events in southern Lake Michigan (DOI 10.1029/2003JC001955)
- Occurence of unfrozen ground in Finland
- The role of horizontal boundaries in parameter sensitivity and decadal-scale variability of coarse-resolution ocean general circulation models
- Detecting long-term variations in precipitation in the southeastern iberian peninsula
- Equitable skill scores for categorical forecasts
- Mesoscale plateau vortex revealed using the scale splitting method
- Field observations of carbonyl sulfide deficit near the groud : possible implication of vegetation
- ORIGIN OF LOW-FREQUENCY [INTRASEASONAL] OSCILLATIONS IN THE TROPICAL ATMOSPHERE. PART 2 : STRUCTURE AND PROPAGATION OF MOBILE WAVE-CISK MODES AND THEIR MODIFICATION BY LOWER BOUNDARY FORCINGS
- ERROR STRUCTURE OF MULTIPARAMETER RADAR AND SURFACE MEASUREMENTS OF RAINFALL. PART I : DIFFERENTIAL REFLECTIVITY
- QUANTITATIVE AND QUALITATIVE EVALUATION OF A THREE-DIMENSIONAL MESOSCALE NUMERICAL MODEL SIMULATION OF A SEA-BREEZE IN COMPLEX TERRAIN
- A DIFFERENT APPROACH TO WORST MONTH RAIN STATISTICS : THEORY AND EXPERIMENTAL RESULTS
- ROLE DE LA VISCOSITE DANS LES ONDES DE RELIEF
- SEARCH FOR ACID SNOW IN NORTH-WEST AFRICA
- A TEST OF A LAPSE RATE / WIND SPEED MODEL FOR ESTIMATING HEAT ISLAND MAGNITUDE IN AN URBAN AIRSHED
- A SPACE-TIME ANALYSIS OF TROPOSPHERIC PLANETARY WAVES IN THE NORTHERN HEMISPHERE
- COMMENTS < ON THE IMPORTANCE OF PRECISION FOR SHORT-RANGE FORECASTING AND CLIMATE SIMULATION >
- Kinetic limitations on cloud droplet formation and impact on cloud albedo