Sea level rise in New Zealand

Sea level rise in New Zealand poses a significant threat to many communities, including New Zealand's larger population centres, and has major implications for infrastructure in coastal areas. In 2016, the Royal Society of New Zealand stated that a one-metre rise would cause coastal erosion and flooding, especially when combined with storm surges.[1][2] Climate scientist Jim Salinger commented that New Zealand will have to abandon some coastal areas when the weather gets uncontrollable.[3] Twelve of the fifteen largest towns and cities in New Zealand are coastal with 65% of communities and major infrastructure lying within five kilometres of the sea.[4][5] The value of local government infrastructure that is vulnerable to sea level rise has been estimated at $5 billion. As flooding becomes more frequent, coastal homeowners will experience significant losses and displacement. Some may be forced to abandon their properties after a single, sudden disaster like a storm surge or flash flood or move away after a series of smaller flooding events that eventually become intolerable. Local and central government will face high costs from adaptive measures and continued provision of infrastructure when abandoning housing may be more efficient.[6]

The results of studies from a programme called NZ Searise released in 2022, indicate that for some parts of New Zealand, the apparent sea level rise will be twice as fast as previously predicted.  This is because of the combined effect of absolute rise in sea level with gradual subsidence of ground levels. [7] In some parts of Wellington, the land is subsiding by 3–4 mm per year, leading to an apparent 30 cm of sea-level rise in 18 years. By 2040, this is forecast to cause inundations every year that are equivalent to a 1-in-100 year event in 2020.[7]

Twentieth century

An analysis in 2004 of long term records from four New Zealand tide gauges indicated an average rate of increase in sea level of 1.6 mm a year for the 100 years to 2000, which was considered to be relatively consistent with other regional and global sea level rise calculations when corrected for glacial-isostatic effects.[8] One global average rate of sea-level rise is 1.7 ± 0.3 mm per year for the 20th century (Church and White (2006).[9] Another global average rate of sea-level rise is 1.8 mm/yr ± 0.1 for the period 1880–1980.[10]

A 2008 study of cores from salt-marshes near Pounawea indicated that the rate of sea level rise in the 20th century, 2.8 ± 0.5 mm per year, had been greater than rate of change in earlier centuries (0.3 ± 0.3 mm per year from AD 1500 to AD 1900) and that the 20th century sea level rise was consistent with instrumental measurements recorded since 1924.[11]

Twenty-first century

Predictions about sea level rise vary considerably. In November 2014, Dr Jan Wright, the Parliamentary Commissioner for the Environment released a report titled Changing climate and rising seas: Understanding the science[12] which says that the sea level is ‘locked in’ to rise by about 30 centimetres by 2050. However, a 2016 report published by the Royal Society of New Zealand finds it likely that the sea level around New Zealand will rise by more than a metre by the end of the century and will exceed the global average by 5–10%.[13] Projections of future sea level rise depend on which carbon emission scenario model is used. Research in 2019 based on a two degree increase in temperature, which is scenario consistent with the Paris Agreement, leads to a possible 81 cm rise by 2100. An Australian policy paper published by Breakthrough in May 2019 predicts a three degree rise in temperature leading to a sea level rise as high as three metres.[14]

In 2016, the Royal Society of New Zealand stated that a one-metre rise would cause coastal erosion and flooding, especially when combined with storm surges.[1][2] Climate scientist Jim Salinger commented that New Zealand will have to abandon some coastal areas when the weather gets uncontrollable.[3]

Associate Professor Nancy Bertler, of the Joint Antarctic Research Institute, at Victoria University of Wellington says: "New research suggests that sea level could rise as quickly as four metres per 100 years (or one metre per 25 years). Assuming even a modest global sea level increase of 50 cm by 2100 (IPCC scenario RCP 4.5), the frequency of coastal inundation in New Zealand is predicted to increase by a multiplier of 1000 times."[15]

Rising sea levels will further threaten coastal areas and erode and alter landscapes whilst also resulting in salt water intrusion into soils, reducing soil quality and limiting plant species growth.[16] The Ministry for the Environment says by 2050–2070, storms and high tides which produce extreme coastal water levels will occur on average at least once a year instead of once every 100 years. GNS climate scientist Tim Naish, says in the event of a two-metre rise in sea-level by the end of the century, one-in-100-year flooding event will become a daily event. Naish says: “We are a coastal nation so we are going to get whacked by sea-level rise. In many areas, we have to retreat "which comes with massive disruption and social and economic issues.”

Twelve of the fifteen largest towns and cities in New Zealand are coastal with 65% of communities and major infrastructure lying within five kilometres of the sea.[4] The value of local government infrastructure that is vulnerable to sea level rise has been estimated at $5 billion.[17] As flooding becomes more frequent, coastal homeowners will experience significant losses and displacement. Some may be forced to abandon their properties after a single, sudden disaster like a storm surge or flash flood or move away after a series of smaller flooding events that eventually become intolerable. Local and central government will face high costs from adaptive measures and continued provision of infrastructure when abandoning housing may be more efficient.[6]

In Auckland, the CBD, eastern bays, Onehunga, Māngere Bridge, Devonport and Helensville are the most vulnerable to inundation.[18]

Wellington is anticipating a 1.5 metre rise which could see much of the central city and low-lying suburbs under water. Areas likely to be inundated include the area around Westpac stadium, swathes of land through the central city, as well as lower parts of Oriental Bay, Evans Bay, Kilbirnie, Shelly Bay, Seatoun, the South Coast bays, parts of Petone, Waiwhetu and the eastern bays as well as much of low-lying areas at Mākara Beach, Pāuatahanui, and Kāpiti.[19]

NZ Searise study findings 2022

The results of studies from a programme called NZ Searise released in 2022, indicate that for some parts of New Zealand, the apparent sea level rise will be twice as fast as previously predicted.  This is because of the combined effect of absolute rise in sea level with gradual subsidence of ground levels. [7] In some parts of Wellington, the land is subsiding by 3-4 mm per year, leading to an apparent 30 cm of sea-level rise in 18 years. By 2040, this is forecast to cause inundations every year that are equivalent to a 1-in-100 year event in 2020.[7]

These revised projections cut in half the time that was thought to be available to plan and implement risk management strategies for these vulnerable areas. The current forecast for global sea level rise is for 0.5 m by 2100, but in some parts of New Zealand, the effective rise in sea level could be twice as great by that time, because of the combined effect of gradual land subsidence.[7] Many different parts of the country are affected by the change in forecast sea level rise. For example, because of the effects of gradual land subsidence, Akaroa on Banks Peninsula in Canterbury can expect 30 cm of sea level rise by the year 2040, instead of 2060. The Wairarapa coastline, around the south-east of the North Island, is forecast to experience the largest increases in sea level.[20]

Vulnerable areas

Nelson airport

The NZ SeaRise programme identified Nelson airport as one area of particular vulnerability, with a projected subsidence of 5 millimetres (0.20 in) per year.[21] In February 2018, the approach road to the airport was flooded when the adjoining Jenkins Creek burst its banks during a storm that brought king tides and strong winds. The airport was closed for about one hour.[22] The airport's Chief Executive said that the proposed runway extension would be planned around the latest sea level rise forecast, and that the airport was "here to stay", despite the concerns over the threats posed by sea level rise.[21]

Adaptation plan

In August 2022, the Ministry for the Environment published Aotearoa New Zealand's first National Adaptation Plan, covering the years 2022–2028. The plan includes a range of adaptation options: Avoid, Protect, Accommodate and Retreat.[23]

See also

References
  1. Climate Change Implications for New Zealand. Royal Society of New Zealand. 19 April 2016. ISBN 978-1-877317-16-3. Archived from the original on 23 June 2016.{{cite book}}: CS1 maint: unfit URL (link)
  2. Morton, Jamie (19 April 2016). "Six reasons why you should worry about climate change". New Zealand Herald.
  3. New Zealand will need to abandon some coastal areas – climate change expert, Newshub 9 February 2018
  4. Warne, Kennedy (November–December 2015). "Three feet high and rising". New Zealand Geographic (136). Retrieved 3 May 2022.
  5. "Maps made available to show extent of flooding threats". RNZ. 25 May 2023. Retrieved 25 May 2023.
  6. Insurance, Housing & Climate Adaptation: Current Knowledge & Future Research, Motu Economic and Public Policy Research,
  7. Cardwell, Hamish (1 May 2022). "Sea levels rising twice as fast as thought in New Zealand". RNZ. Retrieved 1 May 2022.
  8. Hannah, John (12 February 2004). "An updated analysis of long-term sea level change in New Zealand". Geophys. Res. Lett. 31 (L03307): L03307. Bibcode:2004GeoRL..31.3307H. doi:10.1029/2003GL019166. S2CID 53465696. Archived from the original on 11 May 2011. Retrieved 25 January 2010.
  9. Church, J. A.; White, N. J. (6 January 2006). "A 20th century acceleration in global sea-level rise". Geophys. Res. Lett. 33 (L01602): L01602. Bibcode:2006GeoRL..33.1602C. CiteSeerX 10.1.1.192.1792. doi:10.1029/2005GL024826. S2CID 129887186.
  10. Douglas, Bruce C. (25 October 2004). "Global Sea Rise: a Redetermination". Surveys in Geophysics. 18 (2–3): 279–292. Bibcode:1997SGeo...18..279D. doi:10.1023/A:1006544227856. S2CID 128387917.
  11. Gehrels, W. Roland; Hayward, Bruce W; Newnham, Rewi M; Southall, Katherine E (2008). "A 20th century acceleration of sea-level rise in New Zealand". Geophysical Research Letters. 35 (L02717): 192–194. Bibcode:2008GeoRL..3502717G. doi:10.1029/2007GL032632.
  12. Changing climate and rising seas: Understanding the science Archived 26 January 2022 at the Wayback Machine, November 2014
  13. Sea levels and sea-level rise, NIWA
  14. Climate change doomsday scenario could start by 2050 if we don't act, report warns, Stuff 6 June 2019
  15. Sea level rise to impact on New Zealanders – report, Science Media Centre, 27 November 2014
  16. "Overview of likely climate change impacts in New Zealand". www.mfe.govt.nz. Ministry for the Environment. Archived from the original on 27 February 2018. Retrieved 28 May 2018.
  17. Coughlan, Thomas (2 May 2022). "NZ can't build its way out of billion-dollar infrastructure hole - Robertson". NZ Herald. Retrieved 2 May 2022.
  18. 2050 climate: Wellington becomes Auckland, Auckland becomes Sydney, NZ Herald, 14 July 2019
  19. Higher sea-level calculations push more of Wellington under water, Stuff 2 August 2019
  20. Law, Tina (1 May 2022). "Sinking coastlines mean parts of Christchurch will feel impact of sea-level rise earlier than expected". Stuff. Retrieved 1 May 2022.
  21. Bradnock, Erin (19 May 2022). "Nelson Airport 'reassessing' future with new sea-level rise data". RNZ. Retrieved 19 May 2022.
  22. Jones, Katy (8 February 2018). "Airport plans unchanged after terminal shut due to storm surge". Stuff. Retrieved 19 May 2022.
  23. "Aotearoa New Zealand's first national adaptation plan". Ministry for the Environment. 3 August 2022. Retrieved 4 August 2022.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.