ingv - istituto nazionale di geofisica e vulcanologia - italy il sistema clima antonio navarra ingv
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Il Sistema Clima
Antonio NavarraINGV
Atmosfera
Oceani
Il Sistema Clima
BIOSFERA
Umidita’ del Suolo
Fiumi
PrecipitazioniEvaporazione
Ghiaccio
Marino
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La Macchina del Clima
Radiazione Solare
Radiazione Terrestre
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La Circolazione Generale
Le differenti teorie della Circolazione Generale da
quella piu’ antica di Hadley(1735) alla visione
moderna di Bergeron (1928)
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)
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.
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.
NAO
North AtlanticOscillation
SahelNordeste
Monsoon
SST SST
Teleconnections
PNAPNA
PNA
PNA
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Michelson-Morley Experiment
Modelli Matematici
OCEANI -- SUOLO -- CRIOSFERA -- BIOSFERA
RAFFR
EDDAME
NTO
RISCALDAM
ENTO
Calore Latente
Str
ess
del V
ento
PIOGGEEVAPORAZIONE
Calore Sensibile
RI FLESSIONEE
MISSIONE
EMISSIONE
ASSORBIMENTO
TRASPORTO
PRESSIONE
Radiazione
Temperatura VaporAcqueo
TRASPORTO
Rad. Solare
Rad. TerrestreVento
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Atmosphere
Laten Heat Flux
Wind Stress
RAINEVAPORATION
Sensible Heat
Temperature
Currents
TRANSPORT
Solar Radiation
Salinity
TRANSPORT
Atmosphericradiation
Density
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Temperatura Globale A1B
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Temperatura Globale A1B
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Precipitazioni
A1B2060/2080
-1980/2000
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Ottimisti
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