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- W4200580360 abstract "The process of supercooling, where turbulent water is cooled below the freezing point, is a critical condition for the formation of suspended frazil and anchor ice in northern rivers. The behaviour of supercooling has been investigated in numerous laboratory studies but there is a comparatively small number of field observations reported in literature. In this study, high-precision water temperature loggers were deployed on three regulated rivers in Alberta, Canada over multiple winters. A total of 696 supercooling events were detected in the recorded temperature time series. The properties of each supercooling event were calculated (e.g., peak supercooling temperature and duration) and analyzed to increase our understanding of the timing, duration and magnitude of supercooling in rivers. The median peak supercooling temperature, duration and cooling rate averaged of all events was −0.013 °C, 4.8 h and − 2.5 × 10−4 °C/min, respectively. Supercooling events with durations of 2 to 14 days were observed to occur relatively frequently which was surprising since the longest event reported in the literature had a duration on the order of 50 h. Preliminary analysis of the longitudinal distribution of supercooling events along the study reaches demonstrated that dam regulation and urbanization may have a significant impact on supercooling in rivers. Comparison of supercooling observed near the left and right banks in one river showed that there were significant differences in the frequency and duration of supercooling events across the channel." @default.
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- W4200580360 date "2022-02-01" @default.
- W4200580360 modified "2023-09-30" @default.
- W4200580360 title "A study of supercooling in rivers" @default.
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- W4200580360 doi "https://doi.org/10.1016/j.coldregions.2021.103455" @default.
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