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• W2788757530 abstract "Abstract. In sea ice, interconnected pockets and channels of brine are surrounded by fresh ice. Over time, brine is lost by gravity drainage and flushing. The timing of salt release and its interaction with the underlying water can impact subsequent sea ice melt. Turbulence measurements 1 m below melting sea ice north of Svalbard reveal anticorrelated heat and salt fluxes. From the observations, 131 salty plumes descending from the warm sea ice are identified, confirming previous observations from a Svalbard fjord. The plumes are likely triggered by oceanic heat through bottom melt. Calculated over a composite plume, oceanic heat and salt fluxes during the plumes account for 6 and 9 % of the total fluxes, respectively, while only lasting in total 0.5 % of the time. The observed salt flux accumulates to 7.6 kg m−2, indicating nearly full desalination of the ice. Bulk salinity reduction between two nearby ice cores agrees with accumulated salt fluxes to within a factor of 2. The increasing fraction of younger, more saline ice in the Arctic suggests an increase in desalination processes with the transition to the “new Arctic”." @default.
• W2788757530 created "2018-03-06" @default.
• W2788757530 creator A5054760569 @default.
• W2788757530 date "2018-02-21" @default.
• W2788757530 modified "2023-10-01" @default.
• W2788757530 title "Observations of brine plumes below melting Arctic sea ice" @default.
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• W2788757530 doi "https://doi.org/10.5194/os-14-127-2018" @default.
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