mai capito il grafico della mjo
The Madden–Julian oscillation (MJO) is the largest element of the intraseasonal (30- to 90-day) variability in the tropical atmosphere. It was discovered in 1971 by Roland Madden and Paul Julian of the American National Center for Atmospheric Research (NCAR). It is a large-scale coupling between atmospheric circulation and tropical deep convection.[1][2] Unlike a standing pattern like the El Niño Southern Oscillation (ENSO), the Madden–Julian oscillation is a traveling pattern that propagates eastward at approximately 4 to 8 m/s (14 to 29 km/h, 9 to 18 mph), through the atmosphere above the warm parts of the Indian and Pacific oceans. This overall circulation pattern manifests itself most clearly as anomalous rainfall.
The Madden–Julian oscillation is characterized by an eastward progression of large regions of both enhanced and suppressed tropical rainfall, observed mainly over the Indian and Pacific Ocean. The anomalous rainfall is usually first evident over the western Indian Ocean, and remains evident as it propagates over the very warm ocean waters of the western and central tropical Pacific. This pattern of tropical rainfall then generally becomes nondescript as it moves over the cooler ocean waters of the eastern Pacific (except over the region of warmer water off the west coast of Central America) but occasionally reappears at low amplitude over the tropical Atlantic and higher amplitude over the Indian Ocean. The wet phase of enhanced convection and precipitation is followed by a dry phase where thunderstorm activity is suppressed. Each cycle lasts approximately 30–60 days. Because of this pattern, the Madden–Julian oscillation is also known as the 30- to 60-day oscillation, 30- to 60-day wave, or intraseasonal oscillation.
ore 1.00 del 08/08/2013
temperatura 31 gradi
umidità 43%
Scusate una info.
Per ora questi primi 24-25 giorni di gennaio a Rimini e dintorni riescono a farlo da podio come gennaio più caldo? avete un po' di dati? grazie
se va come gfs ne fa 1 metro sul mio cavalcavia, più giorni di neve
Ma quando la neve si scioglie, il bianco dove va a finire?
Per portare quella roba sotto le 100h mancano solo 40 run di GFS, c'è da murì màt!!!
Le 3 cose più belle dall'entrata nel forum e nel mondo meteo : i "mammatus" post-temporale, il nevone 2012 e l'ASE..
Ma le carte non le posta più nessuno?
Le 3 cose più belle dall'entrata nel forum e nel mondo meteo : i "mammatus" post-temporale, il nevone 2012 e l'ASE..
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