Freshwater current between Kara, Laptev Seas discovered
The data collected by the scientists in that strait prompted an earlier unknown flow of desalinated water, moving from west to east in late autumn and early winter
TASS, November 8. Russian oceanographers found in the Arctic Ocean a freshwater current that carries waters of the largest Siberian rivers from the Kara Sea to the Laptev Sea. This process prevents excessive desalination of the Kara Sea, thus affecting the nature of ice formation in its waters, the Russian Science Foundation's press service said.
"The discovery of this subglacial current is fundamentally important to have more accurate forecasts of the ice strength in the Northern Sea Route. Take, for example, the ice that forms and grows from desalinated waters - it is 10-15% stronger than the ice formed from salty sea waters," the press service quoted a senior researcher at the Ocean Studies Institute (the Russian Academy of Sciences, Moscow), Roman Sedakov, as saying.
The expert and his colleagues came to this conclusion after winter-spring studies between 2021 and 2023, where they measured the current's speed, temperature and salinity of water in the Kara Sea and the Laptev Sea. The researchers carried out the measurements both off icebreakers and off a floating station anchored in the Vilkitsky Strait that connects the Kara Sea and the Laptev Sea.
The data collected by the scientists in that strait prompted an earlier unknown flow of desalinated water, moving from west to east in late autumn and early winter. Thus, fresh waters discharged into the Kara Sea by the Ob and the Yenisei Rivers, the world's two largest northern rivers, were transferred into the Laptev Sea under the influence of the Coriolis force generated by the Earth's rotation, and as a result of the difference in buoyancy between fresh and salty waters.
"Due to the Earth rotation, desalinated waters of lower density are forming under the ice a powerful current along the coast and get carried away eastbound - into the Laptev Sea. Due of this process, in January already, the surface layer in the Kara Sea's central part becomes salty again," the press service quoted Alexander Osadchiev, chief researcher at MIPT (Moscow Institute of Physics and Technology, the Moscow Region's Dolgoprudny city), as saying.
According to the scientists, these periodic changes in the salinity of the Kara Sea and the Laptev Sea affect strongly the nature and strength of the ice formed in them in the autumn-winter period. This should be taken into account when laying icebreaker routes along the Northern Sea Route, as well as when forecasting how the ice cover in the Russian Arctic will change in the changing climate.