Coastal Flooding and Sea Level Rise

Our district has low-lying areas close to the coast that are affected by coastal flooding and sea level rise.

Coastal flooding

Coastal flooding can result in significant inundation of low-lying land close to the coast and is especially likely when storm conditions such as storm surges and large waves coincide with high tides. During these events, low-lying areas with direct connection to the sea can be inundated to significant depths and extent.

Coastal storm surge occurs when low-pressure weather systems affect the coast. The sea level rises in response to falling barometric pressure, and strong onshore winds and waves can pile water up against the coast. These phenomena both contribute to storm surge, that when coinciding with high tides produce higher than normal sea levels known as a storm tide. During storms breaking waves cause the average sea level to rise in the surf zone (known as wave set up), which further contributes to coastal inundation when combined with a storm surge. Breaking waves can also surge up the beach slope (wave run up) well above the prevailing sea levels and contributing to coastal flooding.

Cyclone Fehi was a significant coastal storm inundation event that affected our district on 1 February 2018.  The peak of the storm surge coincided with a very high spring tide and large waves damaged the coastline, and flooded roads, reserves, nearby properties and houses.  Sea level rise will increase the exposure of our coastal land to these type of events, with coastal hazards beginning to impact areas that have not previously been exposed.

The Ministry for the Environment has developed a series of factsheets which provide further information on the different elements of coastal processes. View the factsheets on the Ministry for the Environment website(external link).

Coastal flooding at Māpua and Ruby Bay from ex-tropical Cyclone Fehi (Feb 2018)

Sea level rise 

Since 2004, relative sea level rise at the region’s three tides gauges at Port Nelson, Little Kaiteriteri and Tarakohe was 0.14 - 0.15m (NIWA 2023).

Relative sea level rise is made up of two components - a rise in mean sea level and vertical land movement (VLM). Generally VLM along most of Tasman’s coastline is subsiding (NZSeaRise 2024) which results in a higher sea level in relation to the land. Mean sea level is also rising. The combination of the increase in mean sea level together with the VLM is referred to as relative sea level rise.   

Diagram: Difference in mean sea level shoreline between absolute and local (relative)sea level rise where land subsidence occurs.

Source: Ministry for the Environment. 2022. Interim guidance on the use of new sea-level rise projections. Wellington: Ministry for the Environment

The rate and magnitude of future sea level rise is uncertain, especially later this century and beyond.  Scientists advise that sea levels will continue to rise and that levels are likely to rise at an accelerated rate over time as the earth’s temperature rises, meaning changes could happen sooner than predicted – or there may be changes to emission rates that reduce the rate of warming. Uncertainty is a key message.  What we do know is that rising sea levels will have increasing implications for development and infrastructure in coastal areas along with environmental, cultural and societal effects.

The NZ SeaRise: Te Tai Pari O Aotearoa programme developed an online platform which presents location specific sea-level rise projections (including VLM) out to the year 2300 for every 2km of the coast of Aotearoa New Zealand.  The platform outlines when specific sea level rise increments (in metres above 1995-2014 baseline) could be reached for various projection scenarios of sea level rise for New Zealand, including specific data for Tasman. For example, in Tasman we may expect up to 1.66m or 1.67m sea level rise in our district by the year 2130 (under SSP5-8.5 H+ scenario).

Sea level rise and storm surge assessment

We  have started work on a natural hazards plan change(external link) to the Tasman Resource Management Plan (TRMP).  As part of the process, we are improving our knowledge about local hazards and sharing that information with affected landowners and communities.

We’ve developed a coastal hazards map viewer which illustrates the extent of low-lying coastal land in Tasman Bay and Golden Bay that may be affected by a range of hazards as a result of rising sea levels. Our mapped sea level rise elevations information is based on the Ministry for the Environment’s Coastal Hazards and Climate Change Guidance (2024).(external link)

The map identifies low-lying land that may be impacted for a range of sea level rise scenarios in 0.5m increments up to 2m. It also shows the impacts of sea levels being further elevated from a storm-tide event with a 1% joint probability AEP (annual exceedance probability). A 1% AEP event has a 1% chance of occurring in any year.  

Coastal Hazards map viewer(external link)

The methodology used to develop the coastal hazards information shown on the map viewer is described in the accompanying report: 

Coastal Hazards Assessment in Tasman Bay/Te Tai o Aorere and Golden Bay/Mohua (2019)  (pdf 2 MB) 

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