EventScientists recorded cyclonic eddies beneath landfast ice in summer fjords of the northern Canadian Arctic Archipelago, a setting where wind stress alone cannot generate them. The finding suggests new oceanic processes that could shape regional circulation and sea‑ice dynamics.
Cyclonic eddies were recorded beneath landfast ice in fjords of the northern Canadian Arctic Archipelago, a setting where wind stress alone cannot generate them, underscoring previously unobserved oceanic processes that may influence regional circulation and sea‑ice dynamics during summer.
Scientists observed cyclonic eddies beneath landfast ice in fjords of the Northern Canadian Arctic Archipelago during summer, a phenomenon that cannot be driven by wind stress and offers new insights into high‑latitude ocean circulation.