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Rainey Windayati
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ABSTRACT
The tropical atmospheric phenomenon known as the Madden Julian Oscillation (MJO) is an atmospheric, large scale, eastward propagating circulation anomaly that originates over the Western Indian Ocean, confined to the tropics, and moves at around 5 to 10 ms with return interval from 30 to 60 days. Near global analysis demonstrated that the MJO is a signficant phenomenon that can influence daily rainfall patterns, even at higher latitudes, through interactions with Mean Sea Level Pressure ...
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Jakarta: Pusat Penelitian Oseanografi - LIPI, 2016
575 OSEANA 41:3 (2016)
Artikel Jurnal Universitas Indonesia Library
