Thick sea ice flowing from Arctic Ocean shortening shipping season in Northwest Passage, analysis finds

Northwest Passage routes [image credit: NASA @ Wikipedia]

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The authors say this is ‘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 their analysis they note ‘a false sense of optimism regarding the practical usage of the Northwest Passage from purely climate model based studies.’ Another warmist notion bites the dust but, needless to say, the finger of suspicion points at the usual designated suspects i.e. extra trace gases in the atmosphere. So instead of blaming humans for making the NWP more accessible, the same blame is in effect applied for making it less so. Natural variation can’t get a look-in.
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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, says Phys.org.

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-kilometer section of the routes through the CAA was navigable by a PC 7 class ship (capable of safely traveling 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 five-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).

Full article here.
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Image – Northwest Passage routes [credit: NASA @ Wikipedia]