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NZ’s new flood maps are missing a hidden threat – the water quietly rising from below

Adaptation plans don’t account for groundwater in shallow coastal aquifers, which can rise with sea levels, increasing the risk of flooding and damage.

New Zealand's upcoming nationwide flood maps, set for release next year, will provide the clearest picture yet of regional flood risks. However, the current maps overlook a crucial factor: the water table in shallow coastal aquifers, which fluctuates seasonally and is rising due to sea level changes. Groundwater responds to sea level rise in varying ways.

In areas where the water table rises freely with the sea, it increases groundwater flooding risk, maintaining coastal flows and preventing saltwater intrusion. Conversely, in areas with low, flat terrain, the water table remains constrained, weakening freshwater flow to the coast and raising the risk of saltwater intrusion. While nearly one in five New Zealanders live in low-lying coastal areas, these groundwater dynamics rarely appear in adaptation planning.

Groundwater flooding can damage natural resources, agricultural land, and infrastructure before surface flooding occurs. Raising groundwater levels diminish soil's ability to absorb heavy rainfall, exacerbating surface flooding. Current planning treats groundwater as a static variable, but the reality is a dynamic hazard emerging from below. Integrating groundwater dynamics into national flood models is essential for resilience.

Written by urgent.news from Phys.org's reporting — not their text. Machine-written — may contain errors; check the original before relying on it.

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