Water lapping over the Forsyth Barr Stadium site, parts
of Portsmouth Dr under water and roads crumbling into the sea
on the Otago Peninsula - it is a grim picture painted by a
University of Otago climate change model.
And according to experts, the first signs of climate change -
which some scientists fear could bring a sea-level rise of up
to 1.5m over the next 90 years - may already be emerging in
Dunedin.
Otago Regional Council records highlighted a significant
increase in the intensity of rainfall events in the past
decade, resulting in more flooding within the city, ORC
strategy manager Mike Goldsmith said.
However, the data also showed the overall amount of rain
falling on the city was declining, even as the one-off events
intensified, he said.
There had also been a noticeable drop in the number of frosts
across Otago since 1953, and an increase in the number of
days with temperatures over 25degC, he said.
The changes were consistent with climate-change predictions,
although it could not be confirmed and could yet prove to be
"natural variation", he said.
"That's what's predicted to happen and that's what has
happened over the last few years," he said.
Tidal-gauge data from the Dunedin harbour basin also showed
the sea level was already creeping up at a rate of 1.3mm a
year, according to University of Otago professor John Hannah,
of the national school of surveying.
The rate, based on measurements dating back to 1899, would
equate to just a 12cm increase in Dunedin by 2100, but the
pace was expected to increase, he said.
There were no signs yet the rise was accelerating, but a
University of Otago masters student planned to study that
next year, he said.
Prof Hannah said he, like many climatologists, expected
sea-level rise to speed up as ice in Greenland and the
Antarctic melted more quickly, but a 1.5m rise by 2100 might
be "a little speculative".
He was more comfortable with the latest predictions by the
Intergovernmental Panel on Climate Change (IPCC) in 2007,
which predicted a 0.6m rise by 2100.
University of Otago geochemist Abigail Smith, of the marine
science department, said a computer model she helped develop
highlighted the challenges the city might face.
It showed a 1.5m sea-level rise left unchecked by engineering
or adaptation would have a dramatic affect on parts of the
city's coastline, swamping Portsmouth Dr and the harbour
mouth of the Water of Leith, where the Forsyth Barr Stadium
was being built.
Carisbrook Stadium Trust development director Darren Burden
said the stadium's floor was designed to cope with climate
change and wild weather, with a minimum floor level of 3.7m
above mean sea level.
That meant a 1.5m rise in sea levels would still leave the
stadium floor 2.2m above the water level, and underground
features - such as piles and drainage pipes - were also
designed to handle flood scenarios, he said.
chris.morris@odt.co.nz
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