"A dust devil is caused as heating at the surface causes a warm, thermal updraft. In some cases, this updraft can form a weak circulation," he said.
"If this circulation then crosses a dry area with plenty of dust/sand, this will get caught up in the circulation and that is exactly what's happened here."
Hines said this dust devil was fairly tall and active but was not a tornado, despite looking very similar.
Tornadoes are very uncommon in New Zealand, on average about seven to 10 moderate to strong tornado events are reported each year.
They are typically 20-100m in diameter, track for just a couple of kilometres, and last only a few minutes.
Because they're extremely localised, the damage they cause is very confined to the tornado itself, although the violent winds can fling debris hundreds of metres.
New Zealand's tornadoes pack wind speeds of 115km/h to 180km/h - enough to tear roofs from buildings and tip vehicles.
Although climate change is expected to bring more severe storms to New Zealand over coming decades, it's harder to tell whether that will also mean a higher likelihood of tornadoes.