Abstract:The Madden–Julian Oscillation (MJO) is the leading mode of sub-seasonal
variability in the tropical atmosphere and is a key source of
predictability for extratropical weather through its teleconnection
patterns. These MJO teleconnection patterns can be modulated by the El
Niño-Southern Oscillation (ENSO). However, changes over decadal time
scales are less well understood. ERA5 reanalysis data is used to show
that the boreal winter MJO teleconnection pattern in the northern
hemisphere has changed in recent deca… Show more
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