2005年12月12日 · MJO Task Force Dynamical Model MJO Forecasts; The U.S. CLIVAR program instituted a MJO working group to study and develop diagnostics and metrics related to various components related to the MJO during 2006.

2014年12月31日 · The surface and upper-atmosphere structure of the MJO for a period when the enhanced convective phase (thunderstorm cloud) is centered across the Indian Ocean and the suppressed convective phase is centered over the west-central Pacific Ocean.

A Hovmöller diagram of the 5-day running mean of outgoing longwave radiation showing the MJO. Time increases from top to bottom in the figure, so contours that are oriented from upper-left to lower-right represent movement from west to east.

Outgoing Longwave Radiation (OLR) Anomalies Green shades: Anomalous convection (wetness) Brown shades: Anomalous subsidence (dryness) •While the enhanced convective envelope associated with the MJO became disrupted during late February, the suppressed phase crossed the Maritime Continent and was associated with drier conditions across

Australian Government, Bureau of Meteorology. Madden-Julian Oscillation (MJO) official monitoring page. The MJO is the major fluctuation in tropical weather on weekly to monthly timescales and a major driver of the North Australian Monsoon.

Madden and Julian (1, 2) discovered the most pronounced tropical intraseasonal mode of variability, which is now named as Madden-Julian Oscillation (MJO).The MJO strongly modulates the occurrence of many types of extreme weathers in the global tropics and midlatitudes, including floods, droughts, heavy snow storms, cold surges, heat waves, hurricanes and tropical storms, …

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Once SST anomalies associated with an ENSO are in place, the MJO life cycle is influenced by the SST anomalies. When or if an MJO develops, the simplest effect during El Nino is a farther eastward movement of the convection into the central Pacific whereas during La Nina the convection anomalies barely get into the western Pacific.