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Hail in the tropics has high uncertainty. It occurs, but rarely, and observations are sparse. Satellite data often indicate hail signatures in the tropics, but these can be ice aloft that melts before it reaches the ground. So we tested how often this happens using simulations. 2/4

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Differences between hail/no-hail cases are explained by entrainment theory. Hail cases had more shear to produce wider updrafts, and more humid surroundings. Together this led to less updraft buoyancy dilution and more realisation of instability into vertical motion, supporting large hailstones. 3/4