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Home Science News Climate

Climate change: Thick sea ice flowing from Arctic Ocean shortening shipping season in Northwest Passage

July 11, 2024
in Climate
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Climate change: Thick sea ice flowing from Arctic Ocean shortening shipping season in Northwest Passage
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An increased amount of thick sea ice flowing south from the Arctic Ocean shortened the ice-free shipping season in several parts of the Northwest Passage between 2007 and 2021, according to an analysis in Communications Earth & Environment. The authors suggest this could mean the Northwest Passage is unlikely to become a viable alternative to traditional shipping routes, despite previous hopes that it may become viable due to global warming.

An increased amount of thick sea ice flowing south from the Arctic Ocean shortened the ice-free shipping season in several parts of the Northwest Passage between 2007 and 2021, according to an analysis in Communications Earth & Environment. The authors suggest this could mean the Northwest Passage is unlikely to become a viable alternative to traditional shipping routes, despite previous hopes that it may become viable due to global warming.

The Northwest Passage (NWP) is a commercial shipping route connecting the Atlantic and Pacific Oceans that runs through the Arctic Circle north of North America. Through the Canadian Arctic Archipelago (CAA), it splits into a southern route and a shorter, preferred northern route. The length of the shipping season — the period during which the route is navigable for certain ships — for the entire NWP has been changing due to global warming.

Alison Cook and colleagues used sea ice charts from the Canadian Ice Service to calculate the number of weeks per year that each 10-kilometre section of the routes through the CAA was navigable by a PC 7 class ship (capable of safely travelling through ice up to 70cm thick) between 2007 and 2021. The authors found that the shipping season during this period had significantly shortened in three sections of the northern route — the eastern edge of the Beaufort Sea (a 14-week decrease), and the M’Clure Strait and Viscount Melville Sound (both 5-week decreases). They also found that the M’Clure Strait (as well as the Larsen, Peel, and Viscount Melville Sounds) acted as choke points in the NWP as they experienced between 10 and 25 fewer navigable weeks than other sections.

The authors say that both the choke points and the decreased shipping season length in some areas are the result of an increase in older, thicker ice flowing south from the Arctic Ocean, due to increased melting under climate change of the oldest Arctic sea ice (in the Last Ice Area). This type of ice poses a greater risk to ships than the younger, thinner ice that was previously most common in the CAA. The authors note that their findings could also be problematic for coastal communities in the CAA, as they rely on shipping for food and goods.

***

Springer Nature is committed to boosting the visibility of the UN Sustainable Development Goals and relevant information and evidence published in our journals and books. The research described in this press release pertains to SDG 11 (Sustainable Cities and Communities) and SDG 13 (Climate Action). More information can be found here.



Journal

Communications Earth & Environment

DOI

10.1038/s43247-024-01477-6

Method of Research

Data/statistical analysis

Subject of Research

Not applicable

Article Title

Sea ice choke points reduce the length of the shipping season in the Northwest Passage

Article Publication Date

11-Jul-2024

COI Statement

The authors declare no competing interests.

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