Flooding

Flooding is the most common natural hazard we have to deal with.

Flooding is the most common natural hazard we experience in Tasman. Floods can cause injury and loss of life, damage to property and infrastructure, contamination of water and land, and other environmental impacts. There are two types of flooding: river (fluvial) floods or overland flow floods.

What is river flooding?

River, or fluvial, flooding happens when a river, lake, or stream overflows its banks due to excessive rainfall and inflows from their respective tributaries. The resulting damage can be extensive as the overflow floods low-lying land of the adjacent flood plain.  Additional impacts can arise should flood flows lead to dam failures or breaches in stopbanks.

The severity of a river flood depends on the amount and duration of rainfall in the river's catchment area, how saturated the soil is from previous rainfall events and the catchment’s shape and steepness. In flatter areas, floodwaters tend to spread out and rise more gradually and are shallower. In hilly or mountainous areas, floods can develop rapidly after heavy rainfall and drain quickly with high flow velocities, potentially causing further damage should debris flows occur. Given Tasman’s hilly topography, floods in the District can, and do, develop rapidly.  

Large floods can inundate large areas across their flood plain. For example, in 2010 extreme rainfall resulted in a large flood in the Aorere valley with floodwaters extending right across the entire flood plain in its lower reaches.  
 

Flooding in the Aorere Valley in 2010 (looking upstream towards the Ferntown Bridge). 

What is overland flow flooding? 

Overland flow flooding occurs when intense rainfall accumulates on the ground and flows downhill leading to flooding without the involvement of an overflowing river, lake, or stream. Many people mistakenly believe that flooding only poses a risk if they live near a water body, but overland flow floods can happen anywhere — urban or rural — even in places far away from any water body.  

In urban areas overland flow floods often result in urban stormwater drainage system becoming overwhelmed, causing water to spill onto streets and surrounding properties. The water level typically remains shallow (less than 1 metre in depth), however greater depths can occur where it is constrained and concentrated by such things as buildings, fences and landscaping. Overland flow flooding can cause considerable property damage, and the cost of recovery can be significant for homeowners and communities.

In 2013, an extreme rainfall event (approximately 100mm in 1 hour) caused extensive overland flood flows and surface water ponding across parts of Richmond. More recently, in August 2022 Richmond experienced another, but less severe, rainfall event.  

Flooding in Richmond from the August 2022 severe rainfall event.

Floods can occur very quickly with rapidly rising flood levels accompanied by a rapid, powerful surge of water as a result of heavy rainfall over a short period of time, often in or near elevated terrain where gradients are steeper. Such rapid flooding can also result from the sudden release of water from the failure of an upstream dam. These floods are extremely dangerous and destructive, not only due to the speed of the flow and the sheer force of the water, but also because of the debris it picks up and carries along in its flow. Much of the larger debris is deposited when the gradient flattens out with floodwaters laden with the remaining debris continuing down onto the lower fan. Debris flows can be very destructive, typically arriving in abrupt pulses often described as “walls” of water and debris.  

In 2011, prolonged and extreme rainfall caused flooding in the catchments draining into Ligar Bay and Pohara.  Associated landslides triggered debris flows (rapidly flowing slurry of soil, sand, rocks, boulders and vegetation) which continued down the steeper catchment channels and on to the apex of the outwash fan.

Debris flow in Ligar Bay (December 2011)

Flooding is projected to become more common and severe in the future, as climate change brings more frequent and intense storms.

Where can river and overland flow flooding occur in the district?

Given the District’s hilly topography and weather patterns, large parts of the district are susceptible to overland flow flooding. Thunderstorms can produce very heavy rainfalls locally, resulting in overland flow flooding where they occur. Tasman can also experience long duration, district-wide, high rainfall events impacting the larger catchments and bigger rivers.  Such circumstances occurred in 1983 when many of the district’s catchments, the Tākaka and Motueka in particular, experienced significant flooding.

There are 13 river catchments in our District with varying degrees of management along their lengths. Some rivers, when in flood, have the potential to impact several of our towns to varying degrees. Council manages various stopbanks along the Waimea, Lower Motueka and Riuwaka rivers and Brooklyn Stream for flood protection purposes. However, even with stopbanks in place there is still a residual flood hazard. Stopbanks can overtop or fail during an event, and no form of protection is able to prevent damage in every flooding situation. Read more about river management in Tasman.

Tākaka has no formal flood protection measures. Some limited flood protection to the town is provided by a private stopbank, however much of the town remains exposed to varying degrees of flood hazard.

Stopbanks on the Lower Motueka River were designed and constructed in the late 1950s to provide protection to adjacent farmland from a 2% AEP flood event (a flood with a return period of 50 years on average).  Parts of Motueka town are susceptible to flooding from a breach of the Motueka River stopbanks during a large flood. The Riwaka and Brooklyn areas are susceptible to flooding from multiple sources which include the Riuwaka River, the Brooklyn and Little Sydney Streams, and from a breach of the northern Motueka River stopbanks.

Parts of both Brightwater and Wakefield and surrounding areas are susceptible to flooding from the Wairoa and Wai-iti Rivers, the Mount Heslington and Pitfure Streams and a number of smaller tributaries. Parts of Richmond are susceptible to surface water flooding from the hill catchments above the town.

Council holds information on flooding including historic flood maps, images of past flood events and computer simulations (flood modelling). Council uses this data in our decision-making processes and when providing advice to public.  

Mapping our natural hazards

We’ve started a project to bring together our natural hazards spatial data into a single, online, easy to use, natural hazards map viewer.  While this work is under development, you can view some of our flooding data (and other natural hazards) on our Nelson Tasman Future Development Strategy Map(external link) (under layers/constraints and protected areas).