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An Internet Cable Will Soon Cross the Arctic Circle

The underwater fiber-optic cable would trace the shortest path between Europe and Asia

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Phase 1 Ships from French telecommunications company Alcatel-Lucent are scheduled to install the first section of the undersea cable (which will eventually run between 9,500 and 9,700 miles) from June until September. This 1,150-mile tract should enable the first broadband Internet service for Alaskan Arctic communities ranging from Nome to Prudhoe Bay starting in early 2017. The cable will be buried as deep as 13 feet below the seafloor of the icy Arctic waters [see list of threats below].

Phase 2 The Pacific segment of the Quintillion Subsea Cable System will eventually provide a link from Nome, Alaska, to Japan's existing broadband networks. That will shorten the travel distance of Internet signals connecting the U.S. West Coast with Japan and the rest of Asia.

Phase 3 The last phase of the project will extend the undersea cable east from Prudhoe Bay, Alaska, to the U.K. This final leg will traverse the Northwest Passage as it cuts through the waterways of Canada's Nunavut territory and then crosses the Atlantic Ocean. Once all three phases are complete, the entire cable route will enable Internet data to flow between Europe and Asia at speeds as fast as 30 terabits per second.

Credit:

Map by Pitch Interactive; SOURCE: QUINTILLION NETWORKS

More than a century ago polar explorer Roald Amundsen and his six-man crew became the first to navigate the icy Northwest Passage. This month much larger ships than Amundsen's will retrace parts of the sea route but not as adventurers. Instead they will begin laying an undersea fiber-optic cable meant to connect Asia and Europe by crossing the Arctic Circle—the shortest practical distance yet for Internet signals traveling between the two continents.

Most of the undersea cables that currently form the backbone of the World Wide Web connect the U.S. to Europe and Asia by crossing the Atlantic or Pacific oceans. But climate change and an accelerating loss of Arctic sea ice during summer months have opened the possibility of northern cable routes. “It is more viable for [companies] to propose these new and innovative routes than ever before,” says Nicole Starosielski, a media, culture and communications researcher at New York University and author of the 2015 book The Undersea Network.

In this case, Anchorage-based Quintillion Networks hopes its cable can offer high-speed Internet connections to remote communities in Alaska and Canada for the first time. The cable, which is expected to reduce the lag in transmissions between London and Tokyo, may also offer advantages to stock market traders who want the shortest possible delays on millisecond transactions.


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Many countries would favor less U.S.-centric cable routes and additional backup lines to avoid U.S. surveillance and disruptions in service, Starosielski says. Such political and economic considerations have whetted the world's appetite to fund the installation of new and potentially more costly cable projects. But only time will tell if the Arctic route and other undersea Internet cable ambitions will pay off in the long run.

threats to extant undersea cable

Fish Trawling 40% chance of causing a cable break*

Ship Anchorages 28%

Subsea Earthquakes or Subsidence 8%

Shunt (Electrical) Faults 8%

Amplifier or Branching Unit Failures 4%

Abrasion(wave, seabed, ice) 3%

Other Factors(e.g., sabotage) 9%

*Risk-assessment figures reflect typical threats to cables in the Atlantic and Pacific oceans. For much of the year, ice covering large parts of the Arctic Ocean and surrounding seas may protect this project from the threat posed by fishing vessels.

Jeremy Hsu is a New York City–based writer who has contributed to publications such as Scientific American, IEEE Spectrum, Undark Magazine and Wired.

More by Jeremy Hsu
Scientific American Magazine Vol 314 Issue 6This article was originally published with the title “A Northwest Passage for the Internet” in Scientific American Magazine Vol. 314 No. 6 (), p. 14
doi:10.1038/scientificamerican0616-14