At the top of the world, it’s time to get ready for a new future.
December 2, 2014 — In the winter of 2013–14, hundreds of milk-white birds with luminous yellow eyes and wingspans of up to 5 feet descended on beaches, farmers’ fields, city parks and airport runways throughout southern Canada and the United States.
Traditionally, snowy owls spend most of their time in the Arctic and subarctic regions. But every four years or so when populations of lemmings — among the owls’ favorite foods — cycle downward, a small number of young, inexperienced birds that are less adept than their elders at hunting will fly farther south than they might normally rather than starve to death. No one, however, had seen an irruption as big and as far-reaching as this one, which was the second major such event in North America in three years.
By the first week of December, the big birds were spotted from North Dakota to Maine and from Newfoundland to Bermuda. At one point, owls collided with five planes at Kennedy, LaGuardia and Newark airports.
Snowy owl irruptions are not in themselves a sure sign that something extraordinary is happening in an Arctic world that is warming nearly twice as fast as the global rate. But given the rapid-fire fashion in which similar, unexpected events have been unfolding throughout the circumpolar region, it’s clear that the Arctic we know is coming to an end, and that a new and very different Arctic is taking over.
What happens in the Arctic matters. The ecological, cultural and economic shifts that are currently underway will not only alter the lives of the Inuit, Gwich’in, Nenets and other aboriginal people who live there, they are likely to affect mid-latitude weather patterns, the migrating birds we see, the air we breathe, the fuel we burn and the way in which we transport goods from one continent to another. The question then becomes, how do we understand and manage the end of the Arctic as we know it so we are prepared to deal with the new Arctic that is unfolding?
A Picture of Change
The past 10 years paint a dramatic picture of climate-related changes at the top of the world. First there were massive forest fires that torched a record 4.2 million hectares of trees in the Yukon and Alaska in 2004. Smoke from those fires could be detected all the way to the east coast of Canada and throughout many parts of the contiguous United States. Parts of the Alaska Highway were shut down for days at a time. Alaskans suffered for 15 days when air quality in cities such as Fairbanks was deemed to be hazardous to health by U.S. Environmental Protection Agency standards.
Then it was the collapse of the 9-mile-long, 3-mile-wide, 120-foot-thick Ayles Ice Shelf off the north coast of Ellesmere Island in 2005. Scientist Warwick Vincent likened the collapse, the largest recorded in the Canadian Arctic, to a cruise missile hitting the shelf after it registered as a small earthquake at a seismic station 150 miles away.
In 2006 we learned of the world’s first wild polar bear–grizzly bear hybrid, of further increases in relatively warm Pacific water flowing north through the Bering Strait, of gray whales overwintering in the Beaufort Sea instead of migrating to the California coast and — from the U.S. National Snow and Ice Data Center — news that September sea ice was declining 8.6 percent per decade or 23,328 square miles per year. At the time, some scientists scoffed when NSIDC research scientist Julienne Stroeve predicted that the Arctic Ocean would have no ice in September by 2060. But when Arctic sea ice retreated to another record low a year later, many suggested September ice might be gone by 2040.
Then came 2007 — the year in which it became crystal clear that winter’s freeze was losing its ability to keep up with summer’s melt. A rare, extraordinarily large tundra fire on the north slope of Alaska accounted for 40 percent of the area burned in the state that summer. Avian cholera, a disease that is common in the south but largely absent in the eastern Arctic, killed nearly one-third of the nesting female common eiders at East Bay, home to the largest colony of the species in the region. It was so warm that summer that the Inuit of Grise Fiord, the most northerly civilian community on the continent, were forced to stockpile sea ice for drinking water because runoff from a nearby glacier dried up.
For the third year in a row, hundreds of beluga whales and narwhal made the mistake of staying in the Canadian Arctic longer than they should have because there was still much open water when summer came to an end. In Lancaster Sound alone, Inuit hunters shot more than 600 belugas that would have otherwise drowned as the small pools of open water they were trapped in shrank to nothing over a 10-day period.
But what really made the big melt of 2007 an eye-popping one was the absence of ice in areas where it almost never thaws. The so-called “mortuary” of old ice that perennially chokes M’Clintock Channel in the High Arctic of Canada virtually disappeared that August. The “birthplace” of a great deal of new ice that is manufactured in Viscount Melville Sound to the north was down to half of its normal ice cover. “The ice is no longer growing or getting old,” said John Falkingham, chief forecaster for the Canadian Ice Service.
Extraordinary as the events of 2007 were, the changes that have been brought on by a rapidly warming Arctic have not let up since then. In 2010 and 2012, 100 square miles and 46 square miles, respectively, broke away from the Petermann Glacier in Greenland. The presence of so much warm open water in 2012 — when another record low for sea ice cover was established — fueled an unusually powerful summer cyclone that tore through the Arctic for nearly two weeks.
It wasn’t just sea ice that was being churned up and melted more quickly by these increasingly powerful storms. In the Yukon-Kuskokwim delta in Alaska, which is already vulnerable to rising sea levels, storm surges sent waves of saltwater more than 30 kilometers inland on three occasions between 2005 and 2011. This doesn’t bode well for the million birds that nest in the delta nor for the Chinook (king) salmon, which have been in steep decline in the region for more than a decade. This year’s run of between 71,000 and 117,000 was expected to be as poor as last year’s, which established a record low.
Even among all this, one of the most recent signs of change has been especially alarming. All across the Arctic, scientists have been detecting abnormally high concentrations of methane seeping out of the thawing permafrost. In one spectacular example discovered along Siberia’s Yamal Peninsula in 2014, concentrations of the greenhouse gas 50,000 times higher than the atmospheric average were found to be rising from a 200-foot-deep crater that was formed when a massive sheet of permafrost thawed and collapsed. In another case in Canada’s western Arctic, three of many seeps found in the area were found to be emitting as much greenhouse gases in a year as are emitted by 9,000 average-size cars.
We are already seeing the effects of some of these changes ripple through various ecosystems. Capelin, not Arctic cod, is now the dominant fish in Hudson Bay. Killer whales, once stopped by sea ice, are now preying on narwhals and beluga whales throughout the Arctic Ocean. Pacific salmon of all types are moving into many parts of the Canadian Arctic where they have never been seen before. Polar bears at the southern end of their range are getting thinner and producing fewer cubs than they have in the past. Chukchi Sea walrus are hauling out on land by the tens of thousands, as 35,000 of them did in September 2014 when there was no more sea ice to use as platforms.
The changes that are occurring are circumpolar. In the Norwegian archipelago of Svalbard, fjords on the west coast have not been frozen for several years. Tundra there is being overtaken by shrubs, just as it is in Siberia, Chukotka, Arctic Canada and the north slope of Alaska where barren ground caribou — fixtures on the summer tundra — are dramatically declining. According to the CircumArctic Rangifer Monitoring and Assessment Network, which is run on a voluntary basis by veteran biologists Don Russell, Anne Gunn and others, half of the world’s 23 barren-ground caribou herds that are routinely counted are in decline. Only three, maybe four, are increasing, and they are doing so only modestly. Measured another way by biologists Liv Vors and Mark Boyce, who included the fate of boreal forest and mountain caribou in their survey, 34 of the 43 major herds scientists have studied worldwide in the past decade are in a free-fall.
If the past tells us anything about the future, it’s that there will be many more changes that were not anticipated. A few things, however, we know with some degree of confidence.
First, temperatures will continue to rise, resulting in the Arctic Ocean being seasonally ice-free by 2040 or possibly earlier. Two-thirds of the world’s polar bears will be gone a decade later, as will one-third of the 45,000 lakes in the Mackenzie, one of the largest deltas in the Arctic.
In 2100, when trees and shrubs overtake much of the grasses and sedges on the tundra, what we think of as traditional habitat for barren-ground caribou will have shrunk by as much as 89 percent. Coniferous forests will be replaced by deciduous ones in many places. Some trees will have begun to take root on the south end of the Arctic Archipelago. Most of the polar ice caps on Melville Island will have melted away.
The future is not necessarily all doom and gloom, however.And summer storms in the Arctic will continue to pick up steam as melting ice and warming waters contribute to further rises in sea levels. The pounding these storms inflict on frozen shorelines will accelerate the thawing of permafrost, which currently traps massive amounts of methane. The Arctic Ocean will continue to acidify as its upper surface absorbs the greenhouse gases emitted from both the ground and from the burning of fossil fuels.
The future is not necessarily all doom and gloom, however. There is compelling evidence to suggest that some subarctic and Arctic animals — such as the bowhead whale, the musk ox and the barren-ground grizzly bear — will likely thrive in this warmer world. So, too, may the wood bison, which emerged from the 19th century greatly diminished in the subarctic due to habitat loss and overhunting before animals were reintroduced to parts of the Northwest Territories, the Yukon, Siberia and Alaska. There are even signs that cougars could stage a comeback in a land in which the maneless Beringian lion once preyed on animals such as the saiga antelope.
Still, as daunting as the future Arctic looks to be, it may in fact be much worse. What we think we know about the future of the region may be grossly underestimated because scientists are uncomfortable talking about or putting pen to predictions that are not backed by 95 percent certainty.
Benjamin Abbott and University of Florida researcher Edward Schuur anonymously surveyed climate and fire experts in 2013, asking them how much boreal forest and tundra will burn in the future. Nearly all respondents painted a picture that is much worse than what most experts had publicly claimed. In a “business-as-usual” scenario, they predicted that emissions from boreal forest fires will increase 16 to 90 percent by 2040. Emissions from tundra fires will grow even more rapidly.
As much as we know and think we know about what the future Arctic might look like, it’s what we don’t know that worries scientists like Henry Huntington, co-chair of the National Research Council committee that recently examined emerging research questions in the Arctic. “Many of the questions we’ve been asking are ones we’ve been asking for some time,” says Huntington. “But more and more, there are new questions arising from insights that have been made only in recent years, or phenomena that have only begun to occur.”
Growing Wealth, Shrinking Cooperation
All together, the changes past and present in the Arctic paint a picture of a future unfolding with potentially large economic and geopolitical ramifications.
Receding sea ice, for example, is revealing 22 percent of the undiscovered, technically recoverable hydrocarbon resources in the world, as well as the potential for a commercial fishing industry. It is opening up shipping lanes that are far shorter and more economical than existing routes that must pass through the Panama and Suez canals.
This will prove to be challenging. Most of the Arctic currently belongs to the five coastal Arctic states — the United States, Canada, Russia, Norway, Denmark and Greenland. But a big part of it — the so-called 1.2 million-square-mile “donut hole” in the central Arctic Ocean — does not fall under any country’s jurisdiction.
Until recently, security issues, search and rescue protocols, indigenous rights, climate change, and other environmental priorities were the main concerns of the Arctic Council, an intergovernmental forum that includes the eight voting states bordering the Arctic and several indigenous organizations that have participant status. But the recent admission of China and other major Asian economic powers as observer states is yet another strong sign that the economic development of an increasingly ice-free Arctic is becoming a top priority of nations in the region and beyond.
As this interest in the Arctic’s future wealth grows, willingness to cooperate and compromise may shrink.
The United States, for example, continues to challenge Canada’s claim that the Northwest Passage is part of its inland waters and not an international strait. Nor does the United States recognize Canada’s claim to a small, resource-rich region in the Beaufort Sea. In the meantime, Canada and Denmark have agreed to disagree over the ownership of Hans Island in the eastern Arctic as they continue to work out a tentative agreement on the maritime boundary in the Lincoln Sea. And Russia continues to flex its military might in the Arctic in a way that has NATO allies concerned.
On the positive side, the current process of dividing up the unclaimed territory in the Arctic may well be resolved by protocols set forth by the United Nations Convention of the Law of the Sea. The five coastal Arctic states have been spending hundreds of millions of dollars mapping the Arctic Ocean floor to make a case for extending their territories northward. But the recommendations that will eventually be put forth are likely to come in the distant future, and they are not legally binding.
Alternatively, there may be some hope, because headway has been made in the development of an international fisheries agreement that would protect the waters of the central Arctic Ocean.
The dark horse in all this is China, which as an exporting nation and major energy consumer stands to gain from shorter trade routes through the Arctic and from the energy resources there that remain largely unexploited. It may or may not play along with the Arctic Council’s current efforts to focus on sustainable economic development and environmental protection in the Arctic. A Canadian think-tank — the Macdonald-Laurier Institute — recently suggested that China’s true intentions in the Arctic may amount to “positioning itself to influence heavily, if not outright control, the awarding of select Arctic energy and fishing-related concessions as well as the rules and political arrangements governing the use of strategic waterways now gradually opening due to melting ice.”
With all of this in mind, what should be done?
One clear course of action is to halt the activity giving rise to the change — fossil fuel consumption and the release of methane gas as permafrost thaws and sea ice melts. Given the pace of change and the long lag time, however, there is very little that can be done to stop the Arctic from warming in the short term. Humans have already released so much greenhouse gas that even if we stop right now, it will take centuries to halt or reverse the decline of sea ice cover, the thawing of permafrost, the meltdown of glaciers and the acidification of the Arctic Ocean, which is directly attributable to the increase in emissions.
New economic opportunities may arise from oil and gas developments and commercial shipping, but those economic benefits could be offset by a blowout or shipping accident that could prove to be even more catastrophic than theExxon Valdez disaster and BP’s Deep Water Horizon. Unlike Prince William Sound or the Gulf of Mexico, there is ice in the Arctic and no ports and few runways from which to stage a cleanup. There is also no practical way of separating oil from ice. There is, therefore, a need to develop technologies to increase safety of oil and gas extraction before exploration and extraction proceeds. There is also a need to identify and protect biological hot spots that are vulnerable to this kind of human activity.
One of the biggest challenges in planning for the future is to figure out what the new Arctic (including the subarctic) might look like. Against a backdrop of boreal forest, tundra, permafrost, polar deserts, glaciers, ice caps, mountains, rivers, deltas, sea ice, polynyas, gyres and open ocean, that won’t be easy to do. There are thousands of pieces to this puzzle. They include the 21,000 cold-climate mammals, birds, fish, invertebrates, plants and fungi we know a lot about. They also include countless microbes and endoparasites that remain largely a mystery. Further discoveries of microscopic creatures new to science, such as the picobiliphytes found in the Arctic in 2006, are inevitable.
A rigorous assessment of what the future might look like could help decision-makers understand who the winners and losers will be in a future Arctic and what other surprises we can expect. This will help identify which low-lying Arctic communities need to be shored up, moved or made fire safe. It could guide decision-makers in designing better rules and regulations for pipelines and resource development and for commercial shipping. It could also help decision-makers better understand, predict, mitigate and adapt to both changes in the Arctic itself and trickle-down effects to temperate regions.
This is already being done with some success on a small scale. A program in Old Crow, the most northerly community in the Yukon, for example, successfully paired scientists with community leaders to address the issue of food security in a quickly changing climate. Similarly, in Alaska, the Landscape Conservation Cooperatives have facilitated partnerships between the U.S. Fish and Wildlife Service and other federal agencies, states, tribes, non-governmental organizations, universities and stakeholders within a number of ecologically defined areas.
What the Arctic really needs, in addition to these and other small-scale initiatives, is international cooperation either through an overarching treaty or through a series of binding agreements. The issues are too big, too complex and in many cases too overlapping to be left to individual countries to address. In order for this to happen the role of the Arctic Council needs to be strengthened. Science needs to be funded much better than it has been, the indigenous people of the Arctic must be equal partners in the decision-making process, and non-Arctic countries such as China must be included in the conversation.
The future of the Arctic is not necessarily completely bleak. But if we continue to ignore or underestimate the changes that are taking place in this part of the world, it will, as climatologist Mark Serreze bluntly said in 2009, “bite us [and] bite hard.”
Original Article: http://ensia.com/features/the-end-and-beginning-of-the-arctic/
Edward Struzik has lived in, and spent the better part of the past 35 years exploring and writing about, the circumpolar Arctic. He is currently a fellow at the School of Policy Studies, Queen’s Institute for Energy and Environmental Policy at Queen University in Canada. His next book, Future Arctic: Field Notes from a World on Edge, will be published by Island Press in February 2015.