| Sockeye salmon (Photo: Freshwaters Illustrated) |
Scientists have ‘peeled back the ice’ from 46,000 glaciers between southern British Columbia and south-central Alaska to look at how much potential salmon habitat would be created when underlying bedrock is exposed and new streams flow over the landscape.
Modeling glacier retreat under different climate change scenarios, researchers discovered that, under a moderate temperature increase, the glaciers could reveal potential new Pacific salmon habitat nearly equal to the length of the Mississippi River (6,275 km).
Desirable for salmon, in this case, means low-gradient streams (less than 10% incline) connected to the ocean with retreating glaciers at their headwaters. The team discovered that 315 of the glaciers examined met this criteria.
The international team, led by researchers at Simon Fraser University (Canada) with the University of Birmingham and other organizations, published their findings today in Nature Communications.
Lead author, Simon Fraser University spatial analyst Dr. Kara Pitman comments: “We predict that most of the emerging salmon habitat will occur in Alaska and the transboundary region, at the British Columbia‒Alaska border, where large coastal glaciers still exist. The Gulf of Alaska sub-region is predicted to see the most gains—a 27% increase in salmon-accessible habitat by 2100.