Liste complète des notices publiques
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- Observation des perturbations par radar.
- Annuaire de la Société météorologique de France [1863 - Tableaux météorologiques]
- Rapport sur les observations météorologiques faites en France dans les écoles normales primaires pendant les années météorologiques 1874-1875 et 1875-1876.
- Impact of the Vertical Variation of Cloud Droplet Size on the Estimation of Cloud Liquid Water Path and Rain Detection
- Chemical characteristics of atmospheric aerosols over southwest coast of India
- Operational implementation of a 33-km version of GEM for global medium-range weather prediction at CMC.
- Drag coefficient reduction at very high wind speeds 10.1029/2005JC003114 31 March 2006
- Composition and Chemistry - D13301 - Vertical profiles of HDO/H2O in the troposphere (DOI 10. 1029/2004JD005569)
- Hemispheric asymmetries and seasonal variations of the lowermost stratospheric water vapor and ozone derived from SAGE 2 data
- Problems on physical understanding of snowfall phenomena. [keynote paper]
- A storm surge prediction model for the northern bay of Bengal with application to the cyclone disaster in April 1991
- Measurment of gaseous nitric acid by a Laser-Photolysis Fragment-Fluorescence [LPFF] method in the black forest and at the north sea coast
- Climatology
- Vernal atmospheric mixing in the Antarctic
- VHF RADIO PICTURES OF LIGHTNING FLASHES TO GROUND
- LASER INVESTIGATION OF ATMOSPHERIC POLLUTION IN MOSCOW
- ETAT ACTUEL DE LA MODIFICATION ARTIFICIELLE DU TEMPS. DECLARATION ADOPTEE PAR LE COMITE EXECUTIF A SA TRENTE-TROISIEME SESSION
- Meteorologicheskiye aspekty zagryazneniya atmosfery. Tom I, Svornik dokladov na mezhdunarodnom simpoziume v Leningrade, Mart 1977 (Plenarnyye zasedaniya i sektsiya "TEORIYA ATMOSFERNOY DIFFUZIY I ANALIZ MATERIALOV PO ZAGRYAZNENIYEO VOZDUKHA- CHAST' 1)
- BEITRAG ZU DEN PARAMETERN DES VERTIKALEN WINDPROFILS IN UND UEBER EINEM FICHTENWALD
- AN EXAMPLE OF COMPARISON OF OUTGOING LONGWAVE RADIATION FLUX MEASUREMENTS ACCORDING TO SATELLITE AND BALLOON DATA
