Liste complète des notices publiques
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- Analyse hydraulique de la secheresse 1990 à l'amont du Mas d'Agenais - Annexes
- [Résumé climatique] Mars 2014
- Brown's wind and currents of the northern and southern hemispheres, including chart of the world, showing cold and warm streams of the globe with the law of storms all compiled from the latest data
- Physiologie du mouvement : le vol des oiseaux
- Report on the 4th SPARC general assembly, 31 august-5 september 2008, Bologna, Italy.
- Effects of Solar Activity Cycles in the Atmosphere of the North Atlantic and Europe
- A preliminary assessment of major air pollutants in the city of Suzhou, China
- Acceleration technique for Milankovitch type forcing in a coupled atmosphere-ocean circulation model: method and application for the Holocene
- 3. OBSERVATIONAL AND THEORETICAL STUDIES OF THE DYNAMICS OF MANTLE PLUME-MID-OCEAN RIDGE INTERACTION - Polynas play an important and complex role in climate as "subgridscale" phenomena that couple the deep ocean water and the atmosphere directly through heat and mass transfer
- Vulnerability of Russian forests to climate changes. Model estimation of CO2 fluxes
- Contribution à l'étude de l'énergie solaire en Egypte 2 : la nébulosité et la durée d'insolation
- Characterizing mutiscale variability of zero intermittency in spatial rainfall
- Correction schemes for solar sensors with multiple time constants
- THE INCIDENCE OF OUTBREAKS OF WIDESPREAD THUDERSTORMS IN ENGLAND AND WALES : 1946-1985
- CLIMATIC ASPECTS OF PLANNING IMPOUNDMENTS AND HYDROPOWER OPERATIONS
- OPERATIVNAYA SISTEMA CHISLENNOGO ANALIZA I PROGNOZA POGODY V NATSIONAL NOM METEOROLOGICHESKOM TSENTRE SSHA
- AU SUJET DE L ARTICLE DE REITER R., SLADKOVICH R. ET CARNUTH W. << STRUCTURE FINE ET EXAMEN DES ECHANGES D AEROSOLS SUIVANT LA VERTICALE ENTRE 700 ET 3000 M >> AVEC REPONSES DES AUTEURS
- Agreement between observed rainfall trends and climate change simulations in the southwest of Europe
- A. V. Voznesenskij, klimatolog, geograf.
- Contrôle de longues séries de données climatologiques par une méthode d'homogénéité relative