The La Nina-driven "marine heatwave" that's engulfed the Tasman Sea this summer has delighted beach-goers with warmer water, but likely also had some serious effects on sea life.
Now Kiwi scientists have begun creating a state-of-the-art model, allowing them to forecast, decades into the future, how frequent such events might become as the world warms.
At the core of the Niwa-led project, supported by a $300,000 Marsden Fund grant, is what's known as the subtropical front, or STF.
The front forms the boundary of the warm, salty and nutrient-poor tropical ocean to New Zealand's north, and the cold, fresh, nutrient-rich sub-polar ocean to the south.
The position of the front is highly influenced by currents deep beneath the surface, especially along the Macquarie Ridge off the bottom of the South Island, where water has to pass through narrow channels.