Liste complète des notices publiques
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- Assimilating ASCAT normalized backscatter and slope into the land surface model ISBA-A-gs using a Deep Neural Network as the observation operator: Case studies at ISMN stations in western Europe
- Météo et culture : l'humidité de l'air
- Aerosol and Clouds - D22214 - Pan-Arctic enhancements of light absorbing aerosol concentrations due to North American boreal forest fires during summer 2004 (DOI 10.1029/2006JD007216)
- A numerical simulation of present and future acid deposition in North East Asia using a comprehensive acid deposition model
- Special Section: CRISTA-2 Mission (CRISTA) - CRI 5 Middle atmosphere Kelvin waves observed in Cryogenic Infrared Spectrometers and Telescopes for the Atmosphere (CRISTA) I and 2 temperature and trace species (DOI 10.1029/2001 JD000577)
- Quantummetrical method for measurements of spectra of scattered and reflected solar radiaiton
- Considerations about the influences of topographic reduction coefficient on the evapotranspiration estimation, calculated by hydric balances
- Baroclinic instability in a two-layer, vertically semi-finite domain
- Computer simulation of airborne pyranometer measurements
- DIE HAMBURGER KATASTROPHENFLUT VOM 16./17. FEBRUAR 1962
- FORECASTING TRAJECTORIES OF TROPICAL CYCLONES WITH A NESTED GRID SCHEME ACCORDING TO FGGE DATA
- EVAPORATION OF RAIN FALLING FROM CONVECTIVE CLOUDS AS DERIVED FROM RADAR MEASUREMENTS
- ON THE COOL SKIN OF THE OCEAN
- HISTOIRE MARITIME ET METEOROLOGIE
- COMPARISON OF OBSERVED MIXED-LAYER DEPTHS TO MODEL ESTIMATES USING OBSERVED TEMPERATURES AND WINDS, AND MOS FORECASTS
- TELECONNECTIONS IN THE GEOPOTENTIAL HEIGHT FIELD DURING THE NORTHERN HEMISPHERE WINTER
- A POTENCIALISAN KIHULLHATO VIZMENNYISEG BUDAPEST FOLOTT
- SENSIVITY OF A GLOBAL CLIMATE MODEL TO AN INCREASE OF CO2 CONCENTRATION IN THE ATMOSPHERE
- Development of an automatic continuous analyzer for water-soluble gases in air by combining an artificial lung with an ion chromatograph
- Precipitation measurement correction and quality of corrected data from Valdai hydrological station
