Liste complète des notices publiques
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- Red snow occurrence in Eastern Europe. A case study
- Rapport de stage effectué à Météo-France du 10 décembre au 14 décembre 2018
- A mesoclimatological study on heavy snow-fall. A synoptic study on the mesoscale disturbances
- D02107 - Regional model simulation of North Atlantic cyclones: Present climate and idealized response to increased sea surface temperature (DOI 10.1029/2006JD008213)
- Special Section: International Consortium for Atmospheric Research Transport and Transformation: North America to Europe, Part II - D10S31 - Cloud condensation nuclei closure during the International Consortium for Atmospheric Research on Transport and Transformation 2004 campaign: Effects of size-resolved composition (DOI 10.1029/2006JD007588)
- Spatio-temporal variability of event runoff coefficients
- Modelling monthly streamflows in two Australian dryland rivers: Matching model complexity to spatial scale and data availability
- ENSO and PDG effects on hydroclimatic variation of the upper Colorado river basin
- Proceduri de validare si controlul calitatii datelor aerologice obtinute prin radiosondaj
- Animating satellite imagery
- The saturation of gravity waves in the middle atmosphere. Part 1 : Critique of linear-instability theory
- O ZATUKHANII RASPROSTRANYAYUSHCHIKHSYA PLANETARNYKH VOLN V STRATOSFERE
- VISIBILITY TRENDS - 2. MIDEASTERN UNITED STATES 1948-1978
- BAROCLINIC WAVES AND FRONTOGENESIS. PART 2 : UNIFORM POTENTIAL VORTICITY JET FLOWS - COLD AND WARM FRONTS
- RELATIONSHIP BETWEEN THE STATISTICAL CHARACTERISTICS OF THE SIZE DISTRIBUTION OF AEROSOL PARTICLES AND THE ATTENUATION FACTORS
- O PRICHINAKH VZRYVNOGO NACHALA I GRANITSAKH PASPROSTRANENIYA LETNEGO MUSSONA V INDIJSKOM OKEANE
- A LINEAR MODEL OF A FINITE AMPLITUDE HELMHOLTZ INSTABILITY
- NOTES AND CORRESPONDENCE - SST Observations of the Agulhas and East Madagascar Retroflections by the TRMM Microwave Imager
- Phenological climatic division based on planting dates of potato in Hokkaido.
- The effect of a hadley circulation on the progagation and reflection of planetary waves in a simple one-layer model