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Dryad

Data from: Salinization induced under-ice benthic warming, hypoxia, and reduced spring mixing in a rural lake with low road density

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Sep 03, 2026 version files 1.06 MB

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Abstract

The stratification of ice-covered lakes is currently understood as either cryomictic (mixing near 0 °C) or cryostratified (inverse stratification reaching 4 °C). However, internal or external salt sources may alter these patterns, creating stable stratification with high under-ice bottom water temperatures, a condition we term cryohalostratification, which may lead to anoxia and interference with spring mixing. We measured stratification and water quality over two winters in a rural Canadian Shield lake exposed to a highway. We found high under-ice water temperatures (> 4 °C) and low dissolved oxygen (< 2 mg L-1) because of increases in chloride and sodium. Following a cold winter, stability remained high after ice-off, preventing mixing and prolonging seasonal hypoxia. Lake stability estimates showed that the stability of the lake was enhanced by wind sheltering from the surrounding forest, suggesting that even rural lakes with low road density are susceptible to salinization.