November 18th, 2024

Sea-level rise increasing at faster rate around Aotearoa New Zealand

According to Stats NZ’s recently updated environmental indicator Coastal sea-level rise, relative annual sea levels have risen faster over the last 60 years at four coastal monitoring sites throughout Aotearoa New Zealand.

New Brighton beach, Christchurch, New Zealand
New Brighton beach, Christchurch, New Zealand

Sea levels around Aotearoa New Zealand have risen at a faster rate in recent decades compared with the first half of last century, Stats NZ said today.

According to Stats NZ’s recently updated environmental indicator Coastal sea-level rise, relative annual sea levels have risen faster over the last 60 years at four coastal monitoring sites throughout Aotearoa New Zealand.

“Future climate change projections indicate that sea levels will continue to rise. Rising sea levels affect coastal communities, infrastructure, coastal habitats, and biodiversity,” environmental and agricultural statistics senior manager Michele Lloyd said.

“Sea levels rose faster over the last 60 years, 1961 to 2020, compared with the previous 60 years, 1901 to 1960, at four main sites with records dating back to the 1890s and 1900s: Auckland, Wellington, Lyttelton and Dunedin. The rate of sea level rise has doubled in the 60 years to 2020 at three out of the four sites, Wellington, Lyttelton and Dunedin, compared with the mean rate from 1901 through to 1960.”

Of the locations which have been monitored for over 120 years, Lyttelton near Christchurch showed the highest long-term trend in relative sea-level rise of the four sites at 2.24mm/year (with a margin of error of 0.09mm). Meanwhile, between 1961 and 2020 the largest increase in the rate of annual mean sea-level rise of all the monitoring sites was observed in Wellington.

A view of Wellington harbour: Between 1961 and 2020 the largest increase in the rate of annual mean sea-level rise of all the monitoring sites was observed in Wellington.
A view of Wellington harbour: Between 1961 and 2020 the largest increase in the rate of annual mean sea-level rise of all the monitoring sites was observed in Wellington.

The relative sea-level rise includes any local or regional changes in vertical land movement up or down. Vertical land movement can be caused by sinking or uplift from geological processes such as tectonic and volcanic activity, as well as human activity causing subsidence.

Climate change is one of the main causes of sea-level rise. As greenhouse gas emissions warm the Earth’s atmosphere, heat is absorbed by the ocean. The expansion of sea water as it warms, combined with increased sea volume caused by the melting of glaciers and ice sheets, contribute to sea-level rise.

Data for the coastal sea-level rise indicator is provided by NIWA, the National Institute of Water and Atmospheric Research, and LINZ, Land Information New Zealand. The coastal sea-level rise indicator was last updated in 2019. In addition to the four main long-term monitoring sites, which have records dating back to 1891 (Wellington), 1899 (Auckland and Dunedin), and 1901 (Lyttelton), two sites, Moturiki (Mount Maunganui) and New Plymouth, have been measuring sea level changes since the 1950s.

Stats NZ publishes and updates environmental indicators on the state of New Zealand’s environment including air, marine, fresh water, land, and atmosphere and climate, as part of a joint Environmental Reporting programme with partners the Ministry for the Environment (MfE).