Liste complète des notices publiques
Page 2642/10307
- Program of the International Conference on environmental impact of aerospace operations in the high atmosphere of the American Institute of Aeronautics and Astronautics and the American Meteorological Society, June 11-13, 1973, Denver, Colo
- Les capteurs
- D02108 - What causes the excessive response of clear-sky greenhouse effect to El Niño warming in Community Atmosphere Models? (DOI 10.1029/2007JD009247)
- Pourquoi quantifier la valeur monétaire des bénéfices environnementaux ?
- On the Adequacy of the Weak Wind Wave-Low-Frequency Current Interaction Formulation
- Concerning the upper stratospheric gravity wave and mesospheric cloud relationship over sondrestrom, Greenland
- Budget Cutting and the Value of Weather Services
- Characteristics of surface energy partitioning over snow-Covered first year sea ice in the Canadian arctic archipelago during the spring transition
- Energy balance analysis of nightime leaf temperatures and frost formation in a subalpine environment
- Profiler measurements of vertical velocity fluctuations in the ocean
- Potential predictability assessment for analog long-term forecasting.
- Vliyanie vertikal'noj sostavlyayushchej vetra na rezul'taty temperaturnogo radioakusticheskogo zondirovaniya
- The response of solar radiation in Jubail, Saudi Arabia, to smoke from oil field fires in Kuwait
- Vertical motion and diabatic heating over the indian monsoon region during the bay of Bengal depression of 5-8 July, 1979
- NORTHERN HEMISPHERIC DISTRIBUTIONS OF VERTICAL HEAT FLUXES AT THE EARTH S SURFACE COMPUTED BY THE BULK METHOD
- A WIND-SPEED ANOMALY IN THE SURFACE LAYER IN THE PO VALLEY
- FIZIKA POGRANICHNOGO SLOYA ATMOSFERY
- CARACTERISTICILE DE CALCUL ALE PLOILOR TORENTIALE NECESARE IN DETERMINAREA DEBITELOR MAXIME PE VERSANTI SI IN BAZINELE HIDROGRAFICE MICI DE PE TERITORIUL ROMANIEI
- Observations of double-mixing line structure in the convective boundary layer during the summer monsoon season
- La classification des nuages de Poëy
