Liste complète des notices publiques
Page 1488/10237
- Recent global temperature surge intensified by record-low planetary albedo
- La météorologie aéronautique en régions montagneuses
- The marine atmospheric boundary layer under strong wind conditions: Organized turbulence structure and flux estimates by airborne measurements
- Modeling the climate impact of road transport, maritime shipping and aviation over the period 1860-2100 with an AOGCM
- Impacts of atmospheric modes of variability on Mediterranean Sea surface heat exchange
- C07051 - Algorithm development and validation for satellite-derived distributions of DOC and CDOM in the U.S. Middle Atlantic Bight (DOI 10.1029/2007JC004493)
- Estimation of Regional Evapotranspiration by Combining Aircraft and Ground-Based Measurements
- Report of the sixth meeting of the steering committee on application of LAM to tropical countries [project LAM1]. [Tallahassee, Florida, USA, 26-28 june 1995].
- O pokazatele zasukhi i izbytochnogo ublazhneniya dlya tropicheskikh rajonov severnogo polushariya
- Quantification of nitro- and hydroxylated nitro-aromatic/polycyclic aromatic hydrocarbons in selected ambient air daytime winter samples
- A dynamical explanation for the asymmetry in zonally averaged column abundances of ozone between northern and southern springs
- Energetics of the interaction of eddies with zonal flow according to FGGE data
- HINDCASTS AND DATA ASSIMILATION STUDIES WITH THE WAM MODEL DURING THE SEASAT PERIOD
- AN EXACT CALCULATION OF INFRARED COOLING RATE DUE TO WATER VAPOR
- INFLUENCES OF SNOW COVER AND SOIL MOISTURE ON MONTHLY AIR TEMPERATURE
- COMPARATIVE STUDIES OF NO5-43 CONCENTRATIONS IN SOME TROPICAL RAINS
- SYNOPTIC ORIGIN OF IRISH PRECIPITATION 1970-71
- Vyuziti statistického downscalingu pri konstrukci scénaru zmeny klimatu v ceske republice. Cast 2. Validace a konstrukce scénaru.
- Simulations of cosmogenic 14 CO using the three-dimensional atmospheric model MATCH : effects of 14C production distribution and the solar cycle
- RADARS MILLIMETRIQUES ATMOSPHERIQUES. TYPES ERM 66 ET ERM 86