The Madden-Julian Oscillation (MJO) is an important intraseasonal climate signal which circles the global tropics, but also impacts extratropical weather regimes. Few studies have investigated whether the MJO is a source of regional seasonal climate predictability. The present objective is to determine the extent to which the season and phase (geographic location) of MJO contribute to the frequency of global rainfall anomalies in ensuing seasons. Indices of June-July-August and December-January-February MJO activity for each phase and the El Niño/Southern Oscillation (ENSO) were correlated to three-month averages of rainfall up to a six-month lead time. Field significance was calculated and patterns of the relationships were described. In g...
Impacts of the Madden¿Julian oscillation (MJO) on Australian rainfall and circulation are examined d...
The Maritime Continent archipelago, situated on the equator at 95-165E, has the strongest land-based...
The accuracy of synoptic-based weather forecasting deteriorates rapidly after five days and is not r...
The Madden-Julian Oscillation (MJO) is an important intraseasonal climate signal which circles the g...
The Madden-Julian Oscillation (MJO) is a tropical atmospheric phenomenon, associated with periods of...
This chapter describes the characteristics and sub-seasonal prediction of the Madden-Julian Oscillat...
The accuracy of synoptic-based weather forecasting deteriorates rapidly after five days and is not r...
The accuracy of synoptic-based weather forecasting deteriorates rapidly after five days and is not r...
weather variability across the global tropics. One of the most noticeable features of the MJO is an ...
The accuracy of synoptic-based weather forecasting deteriorates rapidly after five days and is not r...
The Madden-Julian Oscillation (MJO) is a tropical atmospheric phenomenon first recognised in the ear...
[1] The Madden-Julian Oscillation (MJO) is the dominant component of the intraseasonal (30–90 days) ...
The Madden-Julian oscillation (MJO) is the main mode of tropical intraseasonal variations and bridge...
The Maritime Continent archipelago, situated on the equator at 95°–165°E, has the strongest land-bas...
Impacts of the Madden¿Julian oscillation (MJO) on Australian rainfall and circulation are examined d...
Impacts of the Madden¿Julian oscillation (MJO) on Australian rainfall and circulation are examined d...
The Maritime Continent archipelago, situated on the equator at 95-165E, has the strongest land-based...
The accuracy of synoptic-based weather forecasting deteriorates rapidly after five days and is not r...
The Madden-Julian Oscillation (MJO) is an important intraseasonal climate signal which circles the g...
The Madden-Julian Oscillation (MJO) is a tropical atmospheric phenomenon, associated with periods of...
This chapter describes the characteristics and sub-seasonal prediction of the Madden-Julian Oscillat...
The accuracy of synoptic-based weather forecasting deteriorates rapidly after five days and is not r...
The accuracy of synoptic-based weather forecasting deteriorates rapidly after five days and is not r...
weather variability across the global tropics. One of the most noticeable features of the MJO is an ...
The accuracy of synoptic-based weather forecasting deteriorates rapidly after five days and is not r...
The Madden-Julian Oscillation (MJO) is a tropical atmospheric phenomenon first recognised in the ear...
[1] The Madden-Julian Oscillation (MJO) is the dominant component of the intraseasonal (30–90 days) ...
The Madden-Julian oscillation (MJO) is the main mode of tropical intraseasonal variations and bridge...
The Maritime Continent archipelago, situated on the equator at 95°–165°E, has the strongest land-bas...
Impacts of the Madden¿Julian oscillation (MJO) on Australian rainfall and circulation are examined d...
Impacts of the Madden¿Julian oscillation (MJO) on Australian rainfall and circulation are examined d...
The Maritime Continent archipelago, situated on the equator at 95-165E, has the strongest land-based...
The accuracy of synoptic-based weather forecasting deteriorates rapidly after five days and is not r...