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  • La nature a-t-elle toujours horreur du vide ?
  • Improving the representation of stable boundary layers
  • Météosatmer : lettre d'information
  • Tests of an Adjoint Mesoscale Model with Explicit Moist Physics on the Cloud Scale
  • Groundwater dynamics and channel activity as major controls of in-stream nitrate concentrations in a lowland catchment system?
  • Evidence of climate change based on rainfall records in Nigeria
  • Cloudy sky optical paths as derived from differential optical absorption spectroscopy observations
  • On the dynamical aspects of the monsoon boundary layer
  • Heating of a large building complex in relation to weather factors
  • Interhemispheric comparison of the spring circulations in the middle atmosphere
  • The spatial and temporal analysis of the representations of the quasi-biennial oscillation in precipitation over China
  • Comments on "a radar study of the plasma and geometry of lightning"
  • AIR AND SOIL TEMPERATURES DURING AN INTENSE FREEZE IN SHROPSHIRE
  • DIFFUSION IN THE LOWER STRATOSPHERE AS DETERMINED FROM LIDAR MEASUREMENTS OF VOLCANIC AEROSOL DISPERSION
  • SOLITARY ROSSBY WAVES IN ZONAL SHEAR FLOWS AND THEIR INTERACTIONS
  • INFRAKRASNAYA ATMOSFERNAYA USTANOVKA IKAU-1 DLYA ISSLEDOVANIYA SPEKTRAL NOJ PROZRACHOSTI V OBLASTI 2-25 MKM
  • Electricité. Tome 2
  • World weather records : 1971-1980. Volume 2, Europe
  • Air temperature data of Korea. Volume 1 : 1904-1960
  • La statistique en pratique

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