frednz:
I don't think all that many Lower Hutt residents have studied the tsunami evacuation zones map and some panicked unnecessarily and evacuated from "safe" properties.
There is so much fear and confusion in Lower Hutt about this. Even some people on the hills left for higher hills. The are so many people ignorant of the difference between a tsunami on an open coastline and in an enclosed bay.
If a tsunami enters Wellington harbour through the heads or even through Rongotai, it will dissipate quite rapidly because the width of the harbour is much wider than the width of the entrance(s). In fact, the wave will spread around the entire perimeter of the harbour. The harbour perimeter from the Wellington CBD to Eastbourne is over 22km. The entrance through the heads is less than 2km wide. That means the wave energy at landfall be 90% dissipated by at least 90%, i.e. at any point around the harbour the wave energy will average less than 10% of the any point in the original wave entering the harbour. That''s mainly why the disastrous 1906 San Francisco earthquake only produced a 10cm wave in that very large harbour.
The worst case is if resonance occurs, where the frequency of the wave reflections matches that of the harbour then the waves will be amplified just like water sloshing around in a bathtub. That's why so many pools in Hamilton lost a lot of water because resonance amplified the wave height.
[Edit to correct spelling - I don't know why I don't notice typing mistakes until after I post]