PI: Samson Hagos

This field campaign aims to document the radiative and turbulent flux processes that control the strength of the diurnal cycle in precipitation and hence advance understanding of the reason for some MJO convection events to propagate across the MC and others to stall.

When a Maritime Continent Gets in the Way

Diurnal Cycle Interactions with Madden-Julian Oscillation Propagation (DIMOP) / Year of Maritime Convection-ARM