Abstract:During some years, a synoptic scale vortex called the Monsoon Onset
Vortex (MOV) forms within the northward advancing zone of precipitating
convection over the Arabian Sea. The MOV does not form each year and the
reason is unclear. Since the Madden-Julian Oscillation (MJO) is known to
modulate convection and tropical cyclones in the tropics, we examined
its role in the formation of the MOV. While the convective and
transition phases of the MJO do not always lead to MOV formation, the
suppressed phase of the MJ… Show more
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