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Ngahorohoro ā-tai, ā-whanga hoki

Coastal and harbour erosion

Coastal erosion is the loss of land along the coastline due to the action of waves, currents, tides, and other processes.

Erosion can occur suddenly during storms, or gradually over time. The natural action of the sea causes coastlines to advance (accrete) or recede (erode) depending on sediment supply, climate, and ocean conditions. These changes can happen seasonally, annually, or during particular events such as storms. Even over short distances, patterns of erosion and accretion can vary, creating erosion hotspots.

Climate change impacts such as sea level rise and storm intensification will cause the sea to reach further inland, increasing coastal erosion in the future.
 

Current coastal erosion
Future coastal erosion


Currently the dunes are eroded during storms and then grow back to approximately the same position as before. However, as sea level rises with our changing climate the dune system is expected to retreat in land.

Erosion mapping viewer

Our interactive map shows current erosion risk and potential future scenarios with different sea level rise projections out to 2130.

To use the coastal erosion map viewer:

  • Open the viewer using the link below
  • Click on the magnifying glass symbol at the top right
  • Enter the address for the property you would like to see details for

Erosion mapping viewer

Important: These are regional-scale assessments showing probability ranges from 'likely' (66% chance) to 'very unlikely' (5% chance). Professional advice is recommended for property-specific decisions.

Coastal erosion in Tauranga

Tauranga has an extremely varied shoreline that affects how coastal erosion impacts different areas:

Mount Maunganui to Pāpāmoa Dunes

What it is: Dune system built up over 7,000 years backing the open coast

Current status: Relatively stable with slight accretion; significant erosion during storms with recovery over months to years

Future impact: Sea level rise will cause dunes to move upward and retreat landward; storm intensification will increase erosion.

Sane dune erosion in Papamoa

Pāpāmoa Beach dune system

Harbour Cliffs

What it is: Cliffs composed of consolidated ash and river sediments around harbour peninsulas

How erosion works: One-way process through gradual weathering and episodic slips

Future impact: Sea level rise will inundate cliff-base beaches; storm intensification increases wave energy and erosion rates

Te Ariki Park erosion

Cliffs below Te Ariki Park

Low-lying Estuarine Areas

What it is: Salt marshes and mangroves in river/stream estuaries and sheltered harbour areas

Current status: Non-eroding shorelines

Future impact: Sea level rise may cause landward movement of salt marsh; where cliffs prevent inland movement, could lead to salt marsh destruction and subsequent cliff erosion

Matua salt marsh erosion

Matua salt marsh reserve

Technical studies

How our maps were created

Coastal erosion maps identify the probability that coastal land could be impacted by erosion today and with different sea level rise scenarios in the future.

Important: These maps are not forecasts of areas that will be eroded. They are estimates based on the best available data and science of the probability that land could be eroded.

Maps were produced using different models for each shoreline type:

  • Dune erosion model: Accounts for dune height, existing erosion, sea level rise, storm events, and soil characteristics
  • Cliff erosion model: Accounts for rock strength, wave energy, and sea level rise

Latest Studies (2019-2020) Tauranga Harbour and coastal strip

Tauranga Harbour

Coastal Mount Maunganui to Pāpāmoa

Previous studies

2015 coastal erosion study

A high-level coastal erosion study between Tauranga City Council, Western Bay of Plenty District Council and the Bay of Plenty Regional Council was undertaken in 2015. The maps show this risk as either low, medium or high over two timeframes, 20 years (2035) and 100 years (2115).

Tauranga Inner Harbour Erosion Report

2009 coastal erosion mapping update

As part of a wider hazard research programme in 2009 we, along with out advisors, looked at erosion processes specifically along Tauranga’s open coast. As part of the development of the operative district plan at that time, the coastal erosion lines were updated. The analysis considered potential/estimated rates of erosion taking in to account different sea level rise scenarios.  

Coastal erosion hazard zone update (2009) (14mb pdf)

Research pre-2000

In 1994 we commissioned an assessment of coastal erosion hazards from the Centre for Environmental and Resource Studies (CEARS). CEARS recommended establishing a unified programme of hazard management to deal with the risks associated with coastal erosion and inundation.

Then in 1996 we commissioned a comprehensive coastal erosion and inundation hazard risk assessment – dubbed ‘Project Dune Watch’ – along the Mount Maunganui/Pāpāmoa coastline. This risk assessment identified how coastal erosion and inundation could affect land adjacent to the coast within the following 100 years.

Project Dune Watch report (1996) (15mb pdf)

Frequently asked questions

We have been working to understand and manage coastal erosion hazards since 1980. Regular assessments and monitoring carried out since then have sought to better understand coastal erosion hazards and ways in which to manage the associated risks.

The 2009 assessment updated the coastal erosion lines through the development of the operative district plan, taking the effects associated with climate change into consideration. Regular beach profile monitoring and surveying since then has continued to expand our understanding and knowledge.

This latest assessment builds on this knowledge and provides a comprehensive understanding of the extent to which our coastal environment is changing, taking into account sea level rise projections.

These erosion hazard maps identify areas of our coastline that are at risk of erosion by the sea. The maps are an output of modelling by Tauranga City Council and our technical advisors.

The maps show the predicted extent of open coast erosion out to the year 2130 and includes the impact of predicted sea level rise (SLR). Present day coastal erosion hazard areas have been shown for comparison with future erosion and sea level rise scenarios.

The coastal erosion maps illustrate areas likely to be affected by erosion for the open coast based on various time and sea level rise scenarios.

Nine scenarios have been mapped which reflect the likelihood of erosion occurring within the timeframes of present day, 2080 and 2130. 

The scenarios mapped also identify coastal erosion extents as 'likely' or 'extremely unlikely' (but still possible), these scenarios are shown for each timeframe.

Broadly speaking, across the different timeframes, the areas identified as having a 66% probability are considered as ‘likely’ to be affected while areas with 5% probability are ‘extremely unlikely’ to be affected.  

A specific web viewer has been created to allow you to view any property in relation to this hazard. This website includes links to the technical study along with a series of helpful reports and links where further information can be found.

Erosion mapping viewer

The purpose of the Resource Management Act (RMA) is to promote the sustainable management of natural and physical resources. It requires that a number of nationally important matters be recognised which include the management of significant risks from natural hazards. Particular regard must also be given to the effects of climate change. 

The avoidance or mitigation of natural hazards is one of the key functions of council in giving effect to the RMA. A similar requirement also exists for councils under the Building Act, Local Government Act and Civil Defence Emergency Management Act. Consequently, we are required to have a good understanding of the areas potentially at risk from natural hazards to support appropriate land-use planning and development decisions.

The New Zealand Coastal Policy Statement also directs councils to identify areas that may potentially be affected by coastal hazards over a timeframe of at least 100 years. Mapping is the most accepted method to identify hazard-prone areas and provide the greatest level of certainty to the public.

Climate change refers to the changes to the present-day climate associated with the effects of global warming. Climate change is projected to have a significant impact on the land near the coast. This impact will come about especially through sea-level rise and intensification of storm events.

National and regional analysis of climate change impacts have also been carried out by the National Institute of Water and Atmospheric Research (NIWA).

Different sea level rise scenarios reflect different assumptions about ocean warming and the melting of land-based ice.

The four sea level rise scenarios that have been selected for use in this study are based on technical guidance from the Ministry for the Environment on projected sea level rise. 

Historic sea level rise in New Zealand has averaged 1.7 ± 0.1 mm/year with the Bay of Plenty exhibiting a slightly higher rate of 2.1 ± 0.1 mm/year. Climate change is predicted to accelerate this rate of sea level rise in the future.  

NIWA have developed a range of SLR projections for Tauranga based upon recommendations from the Ministry for the Environment (2017) for use in planning processes.

This guidance recommends the use of a range of sea level rise scenarios with a need to take a long-term view towards sea level rise scenarios up to 1.6m. 

It is expected that sea level rise will exacerbate current coastal erosion in terms of scale and frequency of erosion events. It is also likely to increase the frequency of damaging storm/weather events. For example, a modest sea level rise of 0.3m (possibly reached by 2050), is likely to change a present-day rare storm event into an annual event.

We have an obligation to make hazard information we hold available to the public under the Local Government Official Information and Meetings Act 1987. It will be made clear on any Land Information Memorandum (LIM) requested for a property within a hazard area, that council holds information in respect of coastal erosion and for the property which has been derived from a coastal hazard study.

We are required to make information, such as the Coastal Hazard Study, available upon request. We cannot advise you about any effect this information may have on property value or insurance.

It is recommended that professional advice is sought from a property valuation or insurance expert about any questions you may have regarding these matters. Refer to the letter below from Insurance Council New Zealand for more information about insurance.

Information for Property Owners (125kb pdf)

The receipt of this information allows us to continue to plan for subdivision and built development along the open coast and also understand how erosion may occur out to 2130, based upon a range of sea level rise scenarios. This will include consideration of regulatory provisions to manage future development (including intensification) within these risk zones and how to best adapt to changes in hazard information in the future.

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