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At about 30 micrometres in diameter (30 times smaller than a millimetre), ryegrass pollen grains can embed themselves in an eye or a nostril and wreck a hayfever sufferer's day. But they are too large to get into a person's lower airways, the bronchi and bronchioles. Given certain conditions though, they can shatter into particles small enough to be inhaled deeply. In meteorological terms, the north-south band of towering cumulonimbus clouds that swept in from the west across Geelong and the city formed a garden-variety spring thunderstorm, albeit a severe one. "All absolutely normal for the Melbourne climate," says Tarini Casinader, the BOM's Victorian regional director. It was what happened inside the clouds that was exceptional and which largely remains a scientific mystery. Experts hypothesise that masses of intact pollen grains from western pastures were sucked up into the warm updraft of air forming the storm cells. In the humid base of the swirling clouds, the pollen grains exploded. The ruptured pollen returned to earth in the storm's cool downdraft, then was spat out across the ground in the storm's outflow area, or gust front, which was moving just ahead of the storm at 60 kilometres an hour. Philip Taylor's research has led him to think that there might be singularities within a storm cell that can intensify a pollen explosion, including humidity levels and the nature of the electric field, and which may have been responsible for the unprecedented mass nature of the event.