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I think it may have been a low end supercell. Upper flow was NW up to 40kts at 500mb and surface wind was N15kts. That suggests some helicity there. But the environment was cold with 500mb temps around -28C so the steep lapse rates had a lot to do with the waterspouts. I am a bit annoyed I didn't make the 2 hr drive across to the Tauranga as it's a favoured area for this development.Another shot here of a second waterspout taken from Maketu: image source