NZ Weather Research Report
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NZ Weather Research Report
Source pack: Aotearoa’s varied weather
New Zealand’s weather changes quickly because the country lies in the mid-latitude westerly wind belt and is surrounded by ocean. Moist air arriving from the Tasman Sea rises over the Southern Alps, cools and condenses, bringing heavy rain to parts of the West Coast. Air descending on the eastern side is often drier; a warm, dry föhn wind is known locally as a nor’wester. Tropical cyclones can sometimes move south and affect New Zealand as weakened ex-tropical cyclones. Fronts, low-pressure systems and local geography all influence weather. Climate change does not cause every individual storm, but it can shift the odds and increase some risks: a warmer atmosphere can hold more water vapour, contributing to heavier rainfall when conditions are right. Attribution of a particular event needs evidence. Impacts depend on exposure and preparedness as well as the weather itself.
Station
Three-day rainfall (mm)
Peak wind gust (km/h)
West Coast foothills
186
72
Canterbury plains
24
98
Investigate and interpret
Use evidence from the source pack and mini data set. Show your reasoning where useful.
- That is always true for every storm.
- One storm alone proves nothing; attribution needs evidence, although climate change can affect the likelihood or intensity of some hazards.
- Climate change cannot affect rainfall or storms.
- Weather and climate mean exactly the same thing.
- Front
- Föhn wind
- Drought
- Ex-tropical cyclone
- Former tropical cyclone that has moved out of the tropics and changed
- Boundary between air masses with different characteristics
- Warm, dry wind descending on the sheltered side of mountains
- Extended period of unusually low water availability
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