Stratification in the Canadian Arctic Archipelago’s Kitikmeot Sea: Biological and geochemical consequences

W. J. Williams, K. A. Brown, B. A. Bluhm, E. C. Carmack, L. Dalman, S. L. Danielson, B. G. T. Else, R. Fredriksen, C. J. Mundy, L. M. Rotermund, and A. Schimnowski

The Kitikmeot Sea Science Study (K3S) began in 2014. It provides the Canadian High Arctic Research Station with a scientific basis for carrying out integrated, long-term ecological monitoring and research in the Kitikmeot Sea. K3S involves strong partnerships with marine and terrestrial research collaborators in the Kitikmeot.

The K3S has three focus areas:

1) the Pacific-origin estuarine through-flow, which sets the oceanographic structure of the region;

2) the origin and pathways of freshwater that flows into the sea, which influences nutrient balances and stratification; and

3) biological communities that are influenced by tides.

The K3S uses oceanographic and marine biological investigation tools aboard the R/V Martin Bergmann. It also maintains year-round sub-surface oceanographic moorings. Findings from K3S studies during 2014–2017 show the unique nature of the Kitikmeot Sea. Tidal mixing within the region’s many narrow, shallow straits is an important finding. This mixing brings nutrients to the surface, which supports the entire marine food-web.

Further study of the Kitikmeot Sea aims to understand the connectivity of the region’s marine ecosystem and how it functions. This information will complement indigenous knowledge and is useful to northern communities. These communities depend on their marine food-webs for fish and seals and on the sea ice for travel. K3S results are beginning to provide a scientific basis for why the region’s tidal straits have high biological production and dangerous, thin ice. The K3S will continue to collaborate with community partners to investigate these themes throughout the Kitikmeot.

Report a problem or mistake on this page
Please select all that apply:

Thank you for your help!

You will not receive a reply. For enquiries, contact us.

Date modified: