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  • Météomonde n°3 - Septembre 2016
  • C09011 - Differences between observed and a coupled simulation of North Atlantic sea surface currents and temperature (DOI 10.1029/2008JC004848)
  • Analysis of evaporative fraction diurnal behaviour
  • Estimation of Parameters of Physically Based Models of Runoff Generation under Insufficiency of Hydrological Observations
  • Radiative sensitivities for cloud structural properties that are unresolved by conventional GCMs
  • Are equatorial negative lightning flashes more intense than those at higher latitudes ?
  • Meteorological stations network in Croatia and wars
  • Linear and non-linear properties of non-modal periodic frontal waves
  • The impact of high altitude aircraft on the ozone layer in the stratosphere
  • ERS-1. An earth observer that exactly follows its chosen path
  • Reversals in evolving raindrop size distributions due to the effects of coalescence and breakup
  • The odor impact model
  • IMPACT OF NUCLEAR WAR ON WEATHER AND CLIMATE
  • THE USE BY THE METEOROLOGICAL OFFICE OF DECYPHERED GERMAN METEOROLOGICAL DATA DURING THE SECOND WORLD WAR
  • OREGON S SILVER THAW
  • ATMOSFERNAYA TSIRKULATSIYA I PROGNOZ POGODY NA DAL NEM VOSTOKE
  • Generation of Moving Spiral Bands in Tropical Cyclones
  • Qu'est-ce que l'Univers ?
  • Evolution of physical oceanography : scientific surveys in honor of Henry Stommel
  • Le stockage des gaz à effet de serre

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