BRIEF RESEARCH REPORT article

Front. Mar. Sci.

Sec. Physical Oceanography

Volume 12 - 2025 | doi: 10.3389/fmars.2025.1602485

Following a half-century oceanographic data gap in the northern Canadian Arctic Archipelago: Multidecadal variability of the Pacific water throughflow

Provisionally accepted
  • 1University of Manitoba, Winnipeg, Canada
  • 2Freshwater Institute, Fisheries and Oceans Canada (DFO), Winnipeg, Manitoba, Canada
  • 3Department of Climate Sciences, Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research (AWI), Bremerhaven, Bremen, Germany

The final, formatted version of the article will be published soon.

The Canadian Arctic Archipelago (CAA) serves as a major conduit between the Arctic Ocean and the North Atlantic. The Nansen Sound fiord system, which encapsulates Nansen Sound, Greely Fiord, Eureka Sound and several surrounding fiords, forms the northernmost oceanographic passageway through the CAA. Due to hostile ice conditions, the area has been understudied since the original oceanographic surveys were conducted in the 1960s and 1970s. The historic data highlighted a very weak signal of the relatively fresh Pacific-derived water (PW). Here, we present new oceanographic observations, including PW tracers, and contrast them against the historic data. Salinity profiles taken in 2024 show significant freshening as compared to 1976. This freshening is attributed to enhanced presence of PW in the area. We suggest that changes in the Arctic Oscillation impact the export gateways of PW from the Arctic Ocean, with the recent switch to a positive phase enhancing the outflow of cool and less saline PW through the CAA. Overall, this provides a first glimpse into variability of the freshwater flow through the straits of the northern CAA.

Keywords: Canadian Arctic Archipelago (CAA), Pacific-modified polar water, Pacific water tracers, Pacific water pathways, Multidecadal variability

Received: 29 Mar 2025; Accepted: 10 Jul 2025.

Copyright: © 2025 Dmitrenko, Kirillov, Babb, Burgers, Wang, Danilov and Dahl-Jensen. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

* Correspondence: Igor Dmitrenko, University of Manitoba, Winnipeg, Canada

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