Liste complète des notices publiques
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- LES MICROPROCESSEURS. Microcontroleur [Texte imprimé] / Claude Dalet
- Le mystère des pierres qui bougent
- C05022 - Observed physical and environmental causes of scatter in whitecap coverage values in a fetch-limited coastal zone (DOI 10.1029/2007JC004453)
- Composition and Chemistry: D13310 - Simulations of the redistribution of formaldehyde, forrnic acid, and peroxides in the 10 July 1996 Stratospheric-Tropospheric Experiment: Radiation, Aerosols, and Ozone deep convection storm (DOI 10.
- The energy balance experiment EBEX-2000. Part II: Intercomparison of eddy-covariance sensors and post-field data processing methods
- Gravitational Potential Energy Balance for the Thermal Circulation in a Model Ocean
- Aerosols and Clouds - AAC 4. On the optical thickness in the UV range: Analysis of the ground-based data taken at Belsk, Poland (DOI 10.1029/2003JD003571)
- The Rainfall Characteristics of Taiwan
- Two-dimensional Lagrangian model of a rising thermal : application for a liquid water content spatial variability of a warm cumulus cloud
- Estimation of canopy water content in Konza prairie grasslands using synthetic aperture radar measurements during FIFE
- Analisis de las Lluvias torrenciales del 18-19 de junio de 1982, en la region occidental de Cuba
- Die flaechenbezogene eisvolumensumme, eine neue masszahl fuer die bewertung des eiswinters an der ostseekveste schleswig-holsteins und ihr zusammenhang mit dem charakter des meteorologischen winters
- Determination of areal evapotranspiration from satellite data using a temperature/surface fluxes inversion model
- LIGHTNING FATALITIES IN SINGAPORE
- DER SOGENANNTE TEMPERATURABHAENGIGE MESSFEHLER DES LICL-FEUCHTEMESSFUEHLERS UND SEINE RECHNERISCHE KOMPENSATION
- THE INTERPRETATION OF REMOTELY SENSED HIGH CLOUD EMITTANCES
- PREDICTING DOWNSLOPE WINDS
- CLIMATOLOGICAL ASPECTS OF THE TROPICAL CONVECTIVE BOUNDARY LAYER
- Annual and seasonal trends in chemical composition of precipitation in Japan during 1989-1998
- Multiprocessing in meteorological models