Il Sistema Clima Antonio Navarra INGV
Il Sistema Clima Atmosfera Oceani Precipitazioni Evaporazione Ghiaccio Marino Oceani BIOSFERA Fiumi Umidita’ del Suolo
La Macchina del Clima Radiazione Terrestre Radiazione Solare
La Circolazione Generale Le differenti teorie della Circolazione Generale da quella piu’ antica di Hadley(1735) alla visione moderna di Bergeron (1928) Hadley (1735) Bergeron (1928) Ferrel (1856)
Teleconnections NAO PNA Monsoon Sahel SST Nordeste North Atlantic Oscillation Sahel Monsoon Nordeste SST The interactions between atmosphere and oceans in the tropics dominate the variability at interannual scales. The main player is the variability in the equatorial Pacific. Wavetrains of anomaly stem from the region into the mid-latitudes, as the Pacific North American Pattern (PNA). The tropics are connected through the Pacific SST influence on the Indian Ocean SST and the monsoon, Sahel and Nordeste precipitation. It has been proposed that in certain years the circle is closed and and a full chain of teleconnections goes all around the tropics. Also shown is the North Atlantic Oscillation a major mode of variability in the Euro_atlantic sector whose coupled nature is still under investigation.
Michelson-Morley Experiment
OCEANI -- SUOLO -- CRIOSFERA -- BIOSFERA Modelli Matematici Rad. Solare Terrestre Vento Radiazione Stress del Vento RIFLESSIONE EMISSIONE TRASPORTO RAFFREDDAMENTO RISCALDAMENTO TRASPORTO PRESSIONE EMISSIONE ASSORBIMENTO Temperatura Vapor Acqueo Calore Latente PIOGGE Calore Sensibile EVAPORAZIONE OCEANI -- SUOLO -- CRIOSFERA -- BIOSFERA
Numerical Models:Oceans Atmospheric radiation Atmosphere Solar Radiation Sensible Heat Laten Heat Flux EVAPORATION RAIN Salinity Temperature TRANSPORT TRANSPORT Currents Density Wind Stress
Temperatura Globale A1B
Temperatura Globale A1B
Precipitazioni A1B 2060/2080 - 1980/2000
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