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Not into drama of any kind. Life's too short. Enjoy gardening. Walking my little dog and spending time with…. Scorpio51 , Jan , This page presents regional projections as a range of values from a low emissions to a high emissions future. The projected changes are calculated for — referred to as and — compared to the climate of — Compared to , temperatures are likely to be 0. The number of frosts could decrease by around 6 to 17 per year by Rainfall will vary locally within the region.
The largest changes will be for particular seasons rather than annually. Seasonal projections show winter rainfall increasing by 6 to 10 per cent in Whanganui and 7 to 16 per cent in Taumaranui by According to the most recent projections, the Manawatu-Whanganui region is not expected to experience a significant change in the frequency of extreme rainy days as a result of climate change.
A reduction in the number of snow days experienced annually is projected throughout New Zealand, including the Central Plateau. The duration of snow cover is also likely to decrease, particularly at lower elevations. Less winter snowfall and an earlier spring melt may cause marked changes in the annual cycle of river flow in the regions.
Climate change projections for the Manawatu-Whanganui region
Places that currently receive snow are likely to see increasing rainfall as snowlines rise to higher elevations due to rising temperatures. The frequency of extremely windy days in the Manawatu-Whanganui region is not likely to change significantly by There may be an increase in westerly wind flow during winter and north-easterly wind flow during summer.
Future changes in the frequency of storms are likely to be small compared to natural inter-annual variability. Some increase in storm intensity, local wind extremes and thunderstorms is likely to occur. New Zealand tide records show an average rise in relative mean sea level of 1. Let's go.
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