The Athabasca Glacier is just one component of the huge Columbia Icefields above these mountains, which straddle the Alberta-British Columbia boundary, and whose waters end up flowing to the Pacific, the Atlantic (via Hudson Bay), and the Arctic. When first explored the glacier reached the current parking lot but since the mid 1800's has retreated over 1.5 km, and lost much of its volume and depth. In 2014,John Wilmshurst, Jasper National Park's resource conservation manager, said in an interview with The Canadian Press, "We're losing at least five metres (depth) a year on the surface of that glacier. every year"
Photo Credit: Wikicommons

Going, gone! Canada’s western glaciers melting fast.

Canada’s western mountain chains are home to many of the world’s glaciers.

A new study indicates that due to human-influenced climate change, they are melting quickly, and could lose most of their volumes in just a few decades, with up to 70% disappearing completely.

Garry Clarke is the lead author of the research. He is a geophysicist, glaciologist, and professor emeritus in the Department of Earth, Ocean and Atmospheric Sciences at the University of British Columbia.

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Geophysicist, glaciologist, and professor emeritus in the Department of Earth, Ocean and Atmospheric Sciences at the University of British Columbia, Garry Clarke PhD © suppolied

“The 70% (loss) gives a sense of false comfort” G Clarke

For thousands of years the glaciers in the mountains of British Columbia and Alberta have performed a vital ecological function. They store precipitation in winter, and then slowly release it throughout the hot summer. This provides cool fresh water for hundreds of major and minor river systems and lakes throughout the northwest of the continent.

Water for fish, birds, animals, and plants, and in very recent centuries, ranching and farming that helps feed the world.

Without glaciers mitigating effect and water reservoir,  much of the western prairie could be far far drier with a major affect on all life there.

In addition, the rapidly melting (and not recovering) glaciers wil have a noticeable affect on sea level rise.

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This photo taken on Aug. 17, 2014 shows a mostly blue-green lake where an icy white Decker Glacier near Whistler, B.C., used to be. (Jason Krupa © USGS
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This is the same glacier in July 2006, still showing complete ice coverage only a few years earlier © USGC Jason Krupa

Professor Clarke says the situation could actually be worse than the 70% loss indicated in the study. He says the only reason it’s not close to a 100% loss of the provinces glaciers is due to a relatively small area in the mountains in the northwest corner of the province.

The study is the result of ten years work  

In collaboration with researchers at the University of Iceland, the University of Victoria, the University of Northern British Columbia,and the Pacific Climate Impacts Consortium, professor Clarke incorporated the “flow physics” of ice and snow into a computer model of western Canada and its glaciers.

The model was begun at a point 2,000 years ago, and when run to the present day, the figures were compared to actual current figures as a verification of the model, and was shown to accurately predict the current state of the province’s glaciers.

 

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In the Canadian Rocky Mountains, the Columbia Icefield represents an important source of snow and ice melt for the Athabasca, Saskatchewan and Columbia river basins. The Icefield is located between Banff and Jasper National Parks and visited by millions of people each year. Shown are the changes in predicted ice extent for high (greater than 1370 ppm of atmosphericCO2-equivalent; The emission scenarios is referred to as RCP8.5 in the Intergovernmental Panel on Climate Change Fifth Annual Report © G Clarke et al- UBC

Professor Clarke and colleagues then ran the study model into future decades using two IPCC scenarios in a probable and worst case scenario from the latest annual report. Both scenarios portray a “bleak message” he says.

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he Glaciers near Stewart ,in the middle northwest of BC. In the Coast and St Elias Mountains, the Frank Mackie region contains substantial ice cover that straddles the Canada-US border. Glaciers here nourish transboundary, salmon-bearing rivers. Shown is result with the lesser scenario, of 490 ppm of atmospheric CO2-equivalent. Althougn a far lower scenario, it still shows massive ice loss, which would have serious implications for both man and nature. © G Clarke et al- UBC

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Similar to the Columbia Icefield, glaciers under both low and high emission scenarios will continue to retreat. Shown is the model for the greater than 1370 ppm of atmospheric CO2-equivalent © G Clarke et al -UBC

He points out that to the casual observer, there may be little difference to see in photos of a couple of decades ago, and the present, but that is deceptive. While the “area” of a glacier may appear similar, he says they are massively losing volume.

He says that other areas of the world such as South America and  Central Asia are also seeing serious glacier loss with potentially even more serious consequences, and he would like to see the team’s research applied to help project scenarios there.

Abstract of the research in Nature Geoscience

Summary of the paper in Nature Geoscience

 

 

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