Abstract
AbstractActivities of the Madden‐Julian Oscillation (MJO) in boreal winter has recently been found to be stronger in easterly phases of the stratospheric quasi‐biennial oscillation (QBO) than its westerly phases. This QBO‐MJO connection was investigated in this study using a method that identifies individual MJO events by tracking their eastward propagating signals in precipitation. Stronger MJO activities in QBO easterly phases are a consequence of more MJO days, not larger amplitudes of individual MJO events as previously thought. More MJO days come from more MJO events initiated over the Indian Ocean and their longer duration because of a weaker barrier effect of the Maritime Continent on MJO propagation. Zonal heterogeneity exists in the connection between QBO, MJO, and tropical total precipitation in general. This poses a challenge to our current understanding of the MJO dynamics, which has yet to fully include upper‐tropospheric and stratospheric processes.
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Metrics
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Citations
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References
Details
Published
Mar 23, 2018
Vol/Issue
123(6)
Pages
2957-2967
License
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Funding
National Science Foundation Award: NA13OAR310161
National Oceanic and Atmospheric Administration
Cite This Article
Chidong Zhang, Bosong Zhang (2018). QBO‐MJO Connection. Journal of Geophysical Research: Atmospheres, 123(6), 2957-2967. https://doi.org/10.1002/2017jd028171