The Post

Proud Coaster fighting for a low-carbon future

Aotearoa New Zealand’s braided rivers are internatio­nally significan­t, but they’ve been systematic­ally strangled. As climate change threatens to make the problems worse, some academics and scientists are re-imagining what it means to live with rivers, as

- Words: Olivia Wannan Photo: Joseph Johnson

Lisa Tumahai (Nga¯ i Tahu, Tainui) is the chair of Te Ru¯nanga (the board) for Nga¯i Tahu and the deputy chair of the Climate Change Commission. The mother-of-three lives in Hokitika.

LISA TUMAHAI: My parents were both born and bred on the West Coast. We’re very much Coasters. They moved to Christchur­ch in the early 60s, as did a lot of people, for work. We always came back to the West Coast for school holidays.

My parents moved back in 1985 after their children were grown up, doing our own thing.

In my late 20s, I got involved in governance with my ru¯ nanga on the West Coast and have been involved ever since. It’s been an extremely long journey actually, when I think about it. It covers a real spectrum, from the wellbeing of our environmen­t to the wellbeing of our people. It was a calling to serve.

My husband’s family are also from the West Coast, so we moved here in 2016. I’ll never look back. I love it here.

The interim Climate Change Commission was being pulled together and the Government put the call out to iwi for nomination­s. At the time I hadn’t thought about it; then I thought, ‘This is a wonderful opportunit­y.’ I thought I’d have to step up – people have asked me to.

It was such a privilege, a real highlight of my life and my career, to be appointed as a commission­er. A huge challenge: You are there to ensure te ao Ma¯ ori [the Ma¯ ori worldview], matauranga and tikanga Ma¯ ori – those things are considered and demonstrat­ed in the work – and the obligation­s of Te Tiriti o Waitangi, which is written into the legislatio­n.

When you talk to Coasters, they’ll say to you they don’t understand all this climate change hype, because our environmen­t has been changing for the last hundred years. And it has. My dad – he’s now 84 – can tell stories about how different the environmen­t was when he was a child.

The wellbeing of our people requires the wellbeing of our environmen­t. That’s what sustains us and has sustained us for centuries. Our mahinga kai, fishing and food gathering practices, are really important to us. So it’s easy for us to do our part.

I’m having my first grandchild­ren. I’ve been wanting grandchild­ren for such a long time. One of my daughters is having twins. So I’m even more passionate now, thinking about the future for our babies.

Nga¯i Tahu have a guiding principle: Mo¯ ta¯tou, a¯, mo¯ ka¯ uri a muri ake nei. That means: For us, for our children and for the children after us.

Nga¯ i Tahu focused on climate change probably six years ago. We started work on a strategy. We’re an iwi that’s in agricultur­e, in primary industries – we have operations in seafood, forestry, and honey; in tourism and in transport.

Each of our corporate entities is required to have a carbon action plan. Our farming business has a sinking lid to eliminate synthetic fertiliser. Half our farms have cut down use by 30 per cent.

While there’s more work to do, there are some very good people who are making change. They started well before the commission came. It’s very rarely acknowledg­ed.

By the time it started raining high in the Southern Alps, it was already too late for those downstream.

It had been raining for several days in the headwaters of the Rangitata River, between Christchur­ch and Timaru, by the evening of December 6, 2019. A sudden downpour overnight brought the highest river levels observed in two decades, and made it inevitable the river would burst its seams. The question was where.

Like other braided rivers in the region, the Rangitata has been heavily modified. Roads, stop banks, and farmland flank its edges; an enormous line of ponds stapled to its side, designed to capture flood waters for irrigation, resemble an artificial second river.

Before human settlement, the river would have simply flooded, forging a new path for itself. But now it was barricaded with stop banks, its floodplain populated by people with lives and property. The river had been narrowed, giving the kinetic energy of the floodwater­s little opportunit­y to disperse; it could only build strength as it barrelled down the plains.

When the floodwater­s came, they breached the entrance to what used to be the South Branch of the river.

Long ago, the Rangitata River split in two. The southern branch has since dried up, and is now covered in irrigated pasture (the land between the two branches was Rangitata Island, a name which remains).

The floods revived the dead southern branch, which at its peak had more water flowing down it than the main river itself. Some of that water itself broke out, flooding state highway one and cutting off the bottom part of the country for several days. At least two more breaches in the main river added to the flooding.

From the ground, it would have seemed like chaos; floods of water rampaging over the plains, damaging anything in its path. But from above, a different picture was emerging. Environmen­t Canterbury (ECan) staff were photograph­ing the floods from the air, later stitching together the images to create a mosaic of the event.

It showed the floodwater­s were following a predetermi­ned pattern. The flood was itself a river, with twists and braids and tributarie­s, much like the Rangitata itself.

A zombie river, long ago buried beneath asphalt and housing and irrigators, had been revived.

Over thousands of years, the braided rivers of the Canterbury Plains painstakin­gly sketched the landscape they now occupy.

There are more than 150 braided rivers in Aotearoa New Zealand, almost all of which are in the South Island. Their floodplain­s alone span around 250,000ha, more than double the size of Auckland City.

Most notable are the braided rivers that formed the Canterbury Plains, the largest area of flat land in the country: The Rakaia, the Rangitata, the Waimakarir­i, the Waitaki, the Ashley/Rakahuri, and the Waiau.

It is a privileged responsibi­lity, given how few of the world’s rivers are braided. Most rivers, globally speaking, are meandering: They have a single channel, filled with water, that goes from one place to another. Think of the Waikato, the Clutha, the Avon.

Braided rivers are complicate­d, dynamic, destructiv­e; they are three-dimensiona­l, in that water also flows beneath the river, popping up as springs and wetlands which are periodical­ly destroyed and recreated, as if the braided river system is creating its own universe.

Some say braided rivers are better seen as four-dimensiona­l; they move across time, existing in different shapes and forms on the scale of millennia. Where a river ends now may be dozens of kilometres from where it ended centuries ago.

Several specific factors are required for a river to become braided. One is gradient: They must start at high altitude, tumbling steeply to sea-level over a short distance. They also need a constant supply of rock and sediment, which usually comes from young, rapidly eroding mountain ranges like the Southern Alps, which are large enough to create their own weather.

Much of this rock settles on the river beds, forming shingle islands between small, twisting water channels. When it floods, the streams merge into a single channel, carrying the rock and sediment out to sea in a torrent, which is swept back towards the land by the tides to build beaches and protect against coastal flooding.

When the floodwater­s recede, the river may have redesigned itself; shifted its islands, created new braids, destroyed old ones. Then the process begins anew.

Central to this process is flooding.

All rivers flood in the right conditions, but for braided rivers, floods are a defining aspect of their physical function.

‘‘The problem with braided rivers, like any other river, is they periodical­ly break their banks,’’ says Sonny Whitelaw, manager of braided river conservati­on group BRaid (Braided River aid).

‘‘The natural reaction is to say, we’re going to put up these barricades to control the river and prevent them from flooding. And of course, the more you confine it, the more you risk flooding, because you’re trying to carry the same amount of water in a much narrower channel.’’

We sometimes think of river flooding as abnormal; a departure from regular order, a river’s failure to fulfil its implied promise to neatly channel water from one place to another.

But flooding is a feature, not a bug. Floods create and destroy new habitat, and carry sediment from the mountains to the coasts. The tension comes when people, property, and infrastruc­ture are put in the way, justifying further measures to control the river, which can themselves make the problem worse.

That was evident during the catastroph­ic Canterbury floods early this month, which caused widespread damage, mostly from braided river flooding.

It highlights a fundamenta­l tension: Can humans and braided rivers peacefully coexist, particular­ly given the expected impacts of the climate crisis, which, in some ways, will make the rivers more powerful than ever?

When the Waimakarir­i River north of Christchur­ch spilled its banks in 1868, it caused significan­t alarm in the city and its surrounds.

Water flooded much of Christchur­ch,

including Cathedral Square. But the worst damage was done in Kaiapoi, on the northern bank of the river.

As detailed by The Press: ‘‘Kaiapoi, in spite of all the protective works and cuttings constructe­d by the inhabitant­s in the hope of averting the attacks of their dreaded enemy, has, we fear, suffered terribly.’’

The language used by the newspaper was instructiv­e.

To some, the Waimakarir­i is a tupuna, a taonga, a provider of mahinga kai; to the settlers, it was a ‘‘dreaded enemy’’, something to be protected from.

The settlers were not living with the river; they were at war with it. In some ways, they still are.

Communitie­s have long been built along rivers: Floodplain­s are fertile, flat, and easy to develop; the rivers themselves can be harnessed as machines for economic growth.

‘‘The first civilisati­ons on our planet emerged in places like Mesopotami­a – ‘‘between the rivers’’ – so it’s not a new thing,’’ says Professor Gary Brierley, a river scientist and chair of physical geography at the University of Auckland.

‘‘And just like those ancient civilisati­ons fell over because practices were unsustaina­ble, what we’re doing is unsustaina­ble.’’

The problems have become more pronounced as society has moved closer and closer to the rivers, emboldened by the idea they can be controlled.

We can build stop banks to prevent flooding, or capture floodwater­s when they get too high; we can funnel rivers down a particular path, take the gravel out of the riverbed, stuff streams and tributarie­s back into the main channel when they break out.

But some of those practices have undoubtedl­y made the problem worse, and the costs have become increasing­ly harder to justify.

In Christchur­ch, efforts to protect the city from the Waimakarir­i River are costly. The most recent upgrade of the stop bank system cost around $40m. In 2020, insurers nationwide paid out nearly $170m in flooding-related damage (figures which include surface flooding from rain).

Between 1990 and 2012, around 12,000ha of river margin land in Canterbury was claimed by farmers, an analysis by ECan found. Some of this developmen­t has been in the riverbed itself, and has put productive land in the path of river floods and erosion.

Braided rivers have been tapped for water to irrigate farmland, and dammed to generate electricit­y. The flatlands cleared by the rivers have made way for quarries, housing, landfills and other infrastruc­ture, further justifying engineerin­g solutions to protect against floods.

At the same time, wetlands – a crucial buffer against flooding – have been systematic­ally removed.

With climate change, heavy rainfall events are expected to become more severe, particular­ly in the headwaters of the major braided rivers. At the same time, drier conditions on the plains could increase reliance on water, particular­ly for farms, moving us closer to the rivers.

‘‘We’ve got all these factors conspiring to make things more difficult for us, and where we’re at now is only going to be accentuate­d into the future unless we turn some of these things around,’’ Brierley says.

It has prompted a new way of thinking among some river scientists. As the relationsh­ip between rivers and humanity becomes more fraught, how do we co-exist?

Earlier this year, a group of New Zealand academics and scientists co-authored a piece arguing that rivers were being ‘‘strangled’’, and actions were required to undo the damage.

There are many names for this practice; rewilding, reanimatio­n, redynamisa­tion, integrated river management, decolonisa­tion. In the simplest terms, it’s letting a river be a river.

It’s an idea that has gained favour in Aotearoa New Zealand over the last five years. It’s not limited to water scientists; a cross-disciplina­ry group including engineers, ecologists, and geomorphol­ogists have made the argument for letting rivers be rivers.

‘‘There is often a tension between engineerin­g and science,’’ says Dr Heide Friedrich, an associate professor of engineerin­g at the University of Auckland.

‘‘In engineerin­g, we want to put everything in boxes – everything needs to go a certain way. Whereas in science, we understand complexity, holistic assessment, and so on.’’

Engineers have played a significan­t role in river management. By one estimate, stop banks in Aotearoa New Zealand span around 5000km, more than double the length of the country itself. They protect many billions of dollars of assets – not to mention lives – from floods.

But the cost is not only financial. Some of the environmen­tal consequenc­es have not been well understood.

After modest rainfall near Franz Josef in 2016, the Waiho River breached a stopbank and took out a hotel. A few years later, the same river flooded again, destroying a bridge which cost $6m to replace.

It comes after a long period of trying to confine the river, but sediment build-up on the river-bed has increased water levels. The solution has been to build the stop banks higher, which is not financiall­y sustainabl­e. One option is to let the river reclaim its floodplain, which has been converted to pasture, or to move Franz Josef township entirely.

It’s the sort of problem engineers need to grapple with, Friedrich says. Convention­al systems don’t always work.

‘‘In the past, often engineers did a lot of studies, came up with solutions and implemente­d them. But especially when it comes to water environmen­ts, we see there are a lot of unintended consequenc­es,’’ she says.

‘‘Just because there could be an engineerin­g solution doesn’t mean we should use it.’’

‘‘I think the first step is recognisin­g we have created a problem,’’ says Dr Dan Hikuroa, an Earth systems scientist and a senior lecturer in Ma¯ori studies at the University of Auckland.

‘‘A river has been a river mai ra¯no¯, since forever. We’ve created a problem by building on its banks or nearby, restrictin­g it.’’

Hikuroa advocates for a mixture of science and Ma¯tauranga.

River management in Aotearoa New Zealand has been pre-occupied with a river’s component parts; setting acceptable levels for the likes of nitrogen, phosphorus and E. coli, each of which can be independen­tly measured and controlled.

For some river scientists, ma¯ tauranga has clarified questions science has been unable to resolve. What if, instead of seeing a river as a machine to be controlled, something that can be deconstruc­ted, we recognised its mauri and accepted it has a fundamenta­l right to be a river?

The two forms of knowledge are not inherently in conflict, and can be complement­ary. It is an idea, appropriat­ely, informed by the structure of a braided river itself: He awa whiria, two channels weaving and twisting, creating something stronger.

‘‘If you can imagine two strands of knowledge, when you have woven them, they’ll be stronger than those individual strands were on their own,’’ Hikuroa says.

‘‘Each maintains its own integrity within that new thing, whatever it is.

‘‘It’s not just understand­ing the role of nitrogen, or phosphorus, or E. coli – those are discrete pieces of informatio­n that are valuable and valid on their own, but make most sense when considered as part of that holistic system. It’s when we go right down on those small parts, as opposed to looking at the whole system, where things can go awry.’’

It is a view that has already moved beyond academia.

Te Awa Tupua, the law granting the Whanganui River legal personhood, recognises such values explicitly: ‘‘Te Awa Tupua is an indivisibl­e and living whole, comprising the Whanganui River from the mountains to the sea, incorporat­ing all its physical and metaphysic­al elements,’’ the law says.

Similar wording is contained in Te Mana o Te Wai, the concept underlying the Government’s freshwater reforms in 2020: In its hierarchy of obligation­s, the health and well-being of the water comes first, ahead of human and economic needs.

A few years ago, at the Christchur­ch District Court, a farmer was charged with an unusual offence – building a wall in the Selwyn River.

The Selwyn River is braided over some of its length. Much of its observable span is dry, meaning the course of the river channel – particular­ly where it starts and ends – can be hard to determine.

What seemed like a standard prosecutio­n would come to have significan­t ramificati­ons.

The farmer acknowledg­ed building the structure – a bund to protect his land from flooding – without permission, but disputed the claim it was in the riverbed, which would come with a harsher punishment.

He argued the wall was in the floodplain, not the riverbed itself. He was found guilty, but appealed.

The High Court sided with the farmer, as did the Court of Appeal.

It speaks to the confusing way in which rivers are defined. Under the Resource Management Act (RMA), a riverbed is: ‘‘[T]he space which the waters of the river cover at its fullest flow without overtoppin­g its banks’’.

‘‘I feel like I struggle with this every day. We either choose to take a holistic view and say okay, we need to withdraw, we need to enable the rivers to act more like living rivers rather than zombie rivers.’’

SONNY WHITELAW, BRAID

Neither ‘‘fullest flow’’ nor ‘‘banks’’ are defined. So what does it mean?

In bringing the prosecutio­n, ECan had interprete­d it to mean where the river would flow in a one-in-20 or one-in-50 year flooding event, an argument it had successful­ly used before. Under this definition, a river’s floodplain­s would be considered part of the river.

The High Court, however, disagreed. It cited a 1905 case regarding the Hutt River, which defined a river in relation to normal seasonal flow. Under this definition, a river does not include its floodplain; it is a static channel. The court’s interpreta­tion stands, radically changing the definition of some riverbed land.

The biggest consequenc­es are for braided rivers, which are, technicall­y speaking, mostly floodplain, and are clearly not static.

The regular flow of water – the channel – is a minor part of a braided river; it’s only after heavy rain, when the water swells and erodes the river’s banks, changing the river’s course, that the river operates how it should.

As other countries move further towards un-strangling their rivers, legally speaking, New Zealand’s are more strangled than ever (the Government has announced an overhaul of the RMA, but it’s unclear if the definition of a riverbed will change).

‘‘Under the RMA, the definition of a braided river isn’t a braided river – it goes right back to this colonial attitude towards a river being just a channel,’’ says Sonny Whitelaw, of BRaid.

It’s part of a broader problem, she says. How do you define the position of something that constantly moves. ‘‘This is a conundrum we’ve got. The damn things don’t convenient­ly stay in one nice to find place – they’re prone, at a moment’s notice, to just sort of pickup and change location.’’

If you’ve flown into Christchur­ch, you may have seen how this happens. Land around the braided rivers are covered in stretch marks.

They are dead channels and streams, left by the Waimakarir­i River as it shifted north to its current position (thousands of years earlier, the river likely flowed near Te Waihora, south of the city.)

With no interventi­on, the river would likely shift back, over a long-enough time period. With the country’s second-largest city now in the way, protected by 100km of stop banks, that is unlikely to happen.

It is an issue across the lower stretches of every braided river, and the defining challenge for the river reanimatio­n movement.

‘‘I feel like I struggle with this every day. We either choose to take a holistic view and

say okay, we need to withdraw, we need to enable the rivers to act more like living rivers rather than zombie rivers,’’ Whitelaw says.

‘‘But we need to know that we’re going to sacrifice things to do that, and the question is, who pays for it?’’

Ma¯ taraunga shows people can learn to live with rivers. When a flood damaged much of Ma¯ tata township in 2005, among the few buildings that weren’t damaged were marae.

The reason was a pu¯ra¯kau, a narrative applied to the landscape. The river was said to house a taniwha in the form of a lizard, its tail flicking side to side, a sign that people should be cautious.

The story contains a basic geomorphol­ogical fact; the lower channel of the river laterally shifts after floods.

It is one reason for optimism. This is a problem that predates everyone alive today; Perhaps two forms of knowledge, braided, can help ease tensions in the longstandi­ng war between humans and rivers.

‘‘It comes from a way of knowing and being that sees you as part of that system, that sees waterways as ancestors, as tupuna, that says we would prefer to treat them like taonga, not as toilets,’’ Dan Hikuroa says about the move to reanimate rivers.

‘‘That kind of thinking, combined with some cutting edge technical tools where we can be measuring real time E. Coli, nutrient loads, silt loads, rainfall modelling... I think there’s an approach where we can see rivers as more than just a bed, banks, and the water in it, and that’s definitely the way forward for us.’’

For Gary Brierley, the river scientist, answers to some pressing questions have been there all along. It’s now time to put the solutions in place.

‘‘A Ma¯ taraunga Ma¯ ori lens is second nature

to many groups across the country, and it’s frankly, the direction that we need to be going,’’ he says.

‘‘To me, it’s an incredible paradox – we have a good idea from science as to where we want to be, and because of the Treaty obligation­s, if there’s any part of the world where it should be pretty easy to do this, to get on with it, it’s here. And yet we have fallen behind the rest of the world.’’

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 ??  ?? The Rakaia River contains interlocki­ng braids. ALDEN WILLIAMS/ STUFF
The Rakaia River contains interlocki­ng braids. ALDEN WILLIAMS/ STUFF
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 ?? PHOTOS: ALDEN WILLIAMS/STUFF ?? Braided rivers, like the Waimakarir­i, are wide and constantly shifting their banks.
PHOTOS: ALDEN WILLIAMS/STUFF Braided rivers, like the Waimakarir­i, are wide and constantly shifting their banks.
 ??  ?? A bridge crossing the upper reaches of the Waimakarir­i River.
A bridge crossing the upper reaches of the Waimakarir­i River.
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 ??  ?? A quarry (right) taking gravel from the Waimakarir­i River. The river previously flowed where the quarry now sits.
A quarry (right) taking gravel from the Waimakarir­i River. The river previously flowed where the quarry now sits.
 ??  ?? Dead channels south of the Waimakarir­i River show its former path.
GOOGLE EARTH
Dead channels south of the Waimakarir­i River show its former path. GOOGLE EARTH
 ??  ?? An example of farmland encroachin­g onto a braided river.
An example of farmland encroachin­g onto a braided river.

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