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  • Adapted ECC ozonesonde for long-duration flights aboard boundary-layer pressurised balloons
  • High-resolution air-sea coupling impact on two heavy precipitation events in the Western Mediterranean
  • Les poussières
  • Constantes physiques de l'eau
  • Note sur les Vents forts en France
  • Airflows and turbulent flux measurements in mountainous terrain - Part 1. Canopy and local effects
  • Wind tunnel experiment on turbulent diffusion suppression by row covers
  • Forecasting rain for groundnut farmers-how good is good enough ?
  • Observation of submicron aerosol black carbon and visibility degradation in remote area at temperature range from -24° to 20° C
  • Linear and nonlinear stability of quais-two-dimensional jet flows with external friction
  • The great climate debate
  • TERMOFOREZ AEHROZOLEJ PRI MALYKH CHISLAKH KNUDSENA. TEORIYA I EHKSPERIMENT
  • A THREE-DIMENSIONAL NUMERICAL SIMULATION OF SPLITTING SEVERE STORMS ON 3 APRIL 1964
  • EUROPAI HOMERSEKLETI MEZOK INFORMACIOTARTALMA
  • SOME ASPECTS OF TURBULENCE STRUCTURE THROUGH THE DEPTH OF THE CONVECTIVE BOUNDARY LAYER
  • NOTE ON THE EQUATIONS OF LAGRANGE, AND SOME INTEGRALS OF THE BAROTROPIC MODEL
  • Metode si practici de prevederea timpului pentru 3-lo zile
  • The life cycle of baroclinic eddies in a storm track environment
  • A case study of ship track formation in a polluted marine boundary layer
  • LE VENT D'AUTAN

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