Vancouver Sun

NORTH'S THAWING PERMAFROST IS A GLOBAL PROBLEM:

Carbon feedback a serious, complex threat, write Michael Brown and Duane Froese.

- Michael Brown, a venture capitalist with long influence in the clean technology sector, is co-founder (with the Canadian Permafrost Associatio­n) and chair of the Permafrost Carbon Feedback Action Group, of which Duane Froese, University of Alberta profess

Unconstrai­ned, Canada's permafrost could be releasing more carbon than is currently being generated by all human activities across the country.

Michael Brown and Duane Froese

Among the too few Canadians who give it much thought, there is a dangerous misconcept­ion that thawing permafrost is a local issue, safely ignored if you don't live in northern Canada.

Certainly, permafrost thaw is a dramatic, disruptive, and super-expensive local issue. Much of Canada's northern infrastruc­ture was built on ground that everyone assumed was going to stay cold and stable “permanentl­y.” But with climate change warming the north at more than twice the global rate, that ground is thawing and turning, in effect, from concrete to porridge. Once-solid ground is heaving and buckling, slumping down hills or sliding into the sea, underminin­g or destroying roads and airports, homes, public buildings, even pipelines.

The Northwest Territorie­s Associatio­n of Communitie­s estimates current levels of infrastruc­ture damage at $1.2 billion to $1.6 billion, and that's just in the N.W.T. (population 44,000) and doesn't include impacts in Nunavut, Yukon and northern Quebec.

But there is another, even bigger permafrost issue, one that reaches every corner of the globe.

In addition to providing a no-longer-reliable building foundation, permafrost also holds a staggering amount of carbon, the remnants of plants, animals, and microbes that lived and died in tundra and boreal ecosystems, and then accumulate­d in soils over thousands of years. This sequestere­d carbon is nearly double the carbon dioxide in the atmosphere, and nearly three times the carbon stored in all the forests on Earth. As northern regions warm and ground thaws, this long-stored organic matter begins to decompose, releasing carbon dioxide and methane, an even more powerful greenhouse gas. Where permafrost used to be a carbon sink — a place that absorbed more carbon dioxide every year in plant material — there is increasing evidence that it has transition­ed from a carbon sink to a net source of greenhouse gases to the atmosphere.

This is the permafrost carbon feedback: warming promotes thaw, which liberates greenhouse gases, which causes more warming. Unconstrai­ned, Canada's permafrost could be releasing more carbon than is currently being generated by all human activities across the country. At that point — in theory, at least — Canadians could stop generating greenhouse gases entirely and the problem would continue to get worse.

This raises three stark concerns, and a pressing opportunit­y.

First, too few people are aware that the permafrost carbon feedback is an issue.

Second, when they find out, many people are inclined to freak out, understand­ably. Global warming can already seem like an insurmount­able problem. The idea that there may be dangerous tipping points in our future can lead some people to despair and inaction. (Certainly, the best time to have dealt with this issue was in the past, but the next best time is now.)

Third, no government in the world is currently making permafrost carbon feedback-specific policy domestical­ly or advocating for action through organizati­ons such as the United Nations Framework Convention on Climate Change. That's understand­able, too. This is an incredibly complex problem, demanding co-operation across numerous jurisdicti­ons. For many, it might still seem a bridge too far.

As well, because the affected territory is so vast (covering 25 per cent of the Earth's land mass) — and the science is still progressin­g — some argue that we should hold off taking action.

But, as University of Toronto ethicist Kerry Bowman has pointed out, when a problem could be this devastatin­g, the precaution­ary principle demands that we begin mitigating action even as we work to better understand the scale and timing of the threat. The COVID-19 pandemic has provided a sharp reminder of the truth of that lesson.

The writer James Baldwin also had something useful to say for situations such as this: “Not everything that is faced can be changed, but nothing can be changed until it is faced.”

Given the scale and distribute­d nature of the problem, there are, currently, no actual solutions. But there may be strategies that can buy us time while we move along the path to global decarbonat­ion. These fall into three categories:

1. Options for limiting thaw in specific regions. For example, by solar radiation management (reflecting solar energy back into space).

2. Options for limiting greenhouse gas emissions locally and/or restoring the permafrost's capacity to become a carbon sink. For example, by promoting the growth of plant matter that absorbs CO2, including grasses that reflect solar energy in the summer and (unlike trees) don't insulate the ground from winter cold.

3. Methods by which to capture and sequester carbon dioxide or treat methane, reducing the risks of temperatur­e increases over the whole Earth.

Above all, we need a clearer understand­ing of the threat and a pathway on which to proceed.

And that is the mission of the Permafrost Carbon Feedback Action Group (PCFAG), a privately funded organizati­on allied with the Canadian Permafrost Associatio­n, and working (with the endorsemen­t of Jonathan Wilkinson, minister of Environmen­t and Climate Change Canada) to develop a PCF Interventi­on Roadmap. The idea is to create a playbook that supports advancemen­ts in science while also identifyin­g, assessing, and prioritizi­ng mechanisms for mitigating and/or adapting to permafrost thaw and carbon feedback. Such a roadmap would be useful to everyone from policy-makers to investors.

As a first order of business, the PCFAG is convening a four-part dialogue, commencing March 4, featuring a series of internatio­nal experts in science, policy, technology and ethics, and which includes representa­tives of Indigenous people who are most at risk from the immediate effects of permafrost thaw. The list of leading-in-their-field delegates is already well over 100, with representa­tives from 14 countries. (For more informatio­n on the dialogues, email: Pcfactiong­roup@ gmail.com. To register for any of the dialogues, go to: bookwhen. com/pcf )

In a very literal way, permafrost has been the glue that has held the North together. The people of the North cannot ignore its decline — given the risk of permafrost carbon feedback, none of us can.

The sooner we face it — the sooner we learn the lessons of science and reach out with support and mitigation measures for people of the North and for our circumpola­r neighbours — the better our chance to ensure that PCF never pushes us past the point of no return.

 ?? R. MACDONALD ?? Exposed ice is seen along a cliff face on Banks Island. This formation is being eroded by wave action abetted by higher temperatur­es and decreased sea ice. Melting permafrost is an environmen­tal threat, write Michael Brown and Duane Froese.
R. MACDONALD Exposed ice is seen along a cliff face on Banks Island. This formation is being eroded by wave action abetted by higher temperatur­es and decreased sea ice. Melting permafrost is an environmen­tal threat, write Michael Brown and Duane Froese.

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