Liste complète des notices publiques
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- A Perfect Prognosis Scheme for Forecasting Warm-Season Lightning over Florida
- Sensitivity of ozone to summertime climate in the eastern USA: A modeling case study
- Special Section: The Role of Surface Salinity on Upper Ocean Dynamics, Air-Sea Interaction, and Climate (SURFSAL) - SRF 21. Barrier layer formation during westerly wind bursts (DOI 10.1029/2001JC001171)
- Chlorine activation and ozone destruction in the northern lowermost stratosphere
- Regression modelling of hourly NOX and NO2 concentrations in urban air in London.
- High-resolution passive microwave observations of convective systems over the tropical Pacific Ocean.
- Marine surface temperature : observed variations and data requirements
- Tropical deep convection, convective available potential energy and sea surface temperature.
- Dynamics of the Antarctic and Arctic mesosphere and lower thermosphere regions. 2 : the sumidiurnal tide
- Using measured variances to compute surface fluxes and dry deposition velocities : a comparison with measurements from three surface types
- An evaluation of the Darwin area forecast experiment storm occurence forecasts
- The teleconnection analysis on the circulation systems between couthern and northern hemispheres
- Analysis on spatial-temporal variation of the anomalous warm winter in China and the general circulation features in the northern hemisphere
- REPORT OF THE SEMINAR ON PROGRESS IN NUMERICAL MODELLING AND THE UNDERSTANDING OF PREDICTABILITY AS A RESULT OF THE GLOBAL WEATHER EXPERIMENT ; SIGTUNA, SWEDEN, OCTOBER 1984
- A NUMERICAL METHOD FOR INTEGRATING THE KINETIC EQUATION OF COALESCENCE AND BREAKUP OF CLOUD DROPLETS
- ON THE LOCAL DIABATIC FRONTOGENESIS IN THE CENTRAL PART OF QINGZANG GAOYUAN
- RASCHET PERIODA AVTOKOLEBANIJ V VOZDUKHE NAD VODNOJ POVERKHNOST YU V REZHIME SVOBODNOJ KONVEKTSII
- INTRODUCTION TO THE NONLINEAR THEORY OF MESOSCALE METEOROLOGICAL PROCESSES
- Balanced Ocean-Data Assimilation near the Equator
- Sur la possibilité de trouver des ascendances dans les ondes progressantes dans le jetstream pour les vols de distance.