Storm surge waves pound the shore in White Rock, near Vancouver BC. in March 2016. Rising sea level and increased storms both resulting from warming and climate change are already affecting Canada’s huge coastline

Storm surge waves pound the shore in White Rock, near Vancouver BC. in March 2016. Rising sea level and increased storms both resulting from warming and climate change are already affecting Canada’s huge coastline
Photo Credit: Bill Hawke, via CBC

Major scientific study of Canada’s coasts and climate change.

With its three ocean coasts and islands, Canada has the longest coastline in the world, at over 200,000km.

A major and very detailed study on climate change and its effects on the country’s various coastlines has been released this week called, Canada’s Marine Coasts in a Changing Climate,

It details both the current situation and future predictions in coastlines around the country which are already coping with increased temperatures, coastal erosion, flooding, melting sea ice, more frequent and more violent storms, and sea rise.

The Natural Resources Canada report brings together over 1300 scientific studies on climate change sensitivity and risks along Canada’s coastlines

The 280 page report also involves over 60 authors from Canadian universities, federal departments, other levels of government, industry and professional organizations.

Erosion of permafrost coasts in the westernCanadian Arctic: a)= a deep thermoerosional niche undercutting cliff inice-bonded sand and associated block failure following a major storm,Tuktoyaktuk Island, NT...and b)= retrogressive thaw amphitheatresin ice-rich deposits at King Point, YT (edge of lagoon at left).Note massive ice (indicated by white arrow) in lower part of the main headwall, which is ~5 m high.
Erosion of permafrost coasts in the western Canadian Arctic: *A) = a deep thermoerosional niche undercutting cliff in ice-bonded sand and associated block failure following a major storm,Tuktoyaktuk Island, NT…and *B)= retrogressive thaw amphitheatres in ice-rich deposits at King Point, YT (edge of lagoon at left).Note massive ice (indicated by white arrow) in lower part of the main headwall, which is ~5 m high. © A=S.M. Solomon, B=D.L. Forbes, (both Natural Resources Canada

 It also notes that :” Globally, coastal flooding could displace hundreds of millions of people in the current century, with the annual costs for  adaptation measures such as new dike construction, dike maintenance and beach nourishment estimated to be US$25–270 billion per year by 2100”.

RCI-2015- Cape Breton –climate/erosion

RCI-2013- PEI- climate/erosion/landmarks

The report notes some of the greatest changes will be in the Canadian north, saying, “Canada’s northern coastline is vast, representing more than 70% of all Canadian coasts. The region has experienced some of the most rapid climate change anywhere on the globe”.  It goes on to say that, “Many communities have a high sensitivity to climate change impacts, as they are situated on low-lying coasts and have infrastructure built on permafrost, economies strongly linked to natural resources and dependence on land-based harvesting activities”, and that,  “Climate change will exacerbate existing vulnerabilities”.

Collapsed blocks of permafrost near Drew Point Alaska. The USGS reporst shoreline erosion along the Arctic coast ranging from 2 to 18 metres per year.
Collapsed blocks of permafrost near Drew Point Alaska. The USGS reports shoreline erosion along the Arctic coast ranging from 2 to 18 metres per year, similar to what Canadian studies have found elsewhere across Canada’s Arctic coastline. © USGS Alaska Science Center- C Arp

The report shows throughout, the extent to which various regions of the country’s coastline and its millions of inhabitants will be affected in coming years by a changing climate.

It says future planning along coastlines must take climate change into account noting, “it is imperative that future development be undertaken with an understanding of the dynamic nature of the coast and changing coastal risks”.

Additional information- sources

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