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Relation of ice growth rate to salt segregation during freezing of low-salinity sea water (Bothnian Bay, Baltic Sea)

机译:低盐度海水(Bothnian Bay,波罗的海)冻结冰增长速度与盐隔离的关系

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Salt segregation and isotopic fractionation during sea-ice formation can be parameterized as a function of the ice growth rate. We performed a study to investigate if the salt segregation models derived for saline sea-ice studies are pertinent during the growth of Baltic Sea ice in brackish water. We used a time series of ice-salinity profiles and modeled growth rates to examine the relationship between effective salt segregation and growth rate. The results show that models derived for saline sea water are not directly applicable for use in the brackish waters of the Baltic Sea.We derived a simple model for the effective salt segregation in relation to ice growth rate, for a wide range of growth rates, pertinent for use in low-salinity Baltic Sea conditions and in the future development of a Baltic Sea ice salinity model.
机译:在海冰中的盐偏析和同位素分级可以作为冰增长率的函数进行参数化。我们进行了研究以调查用于盐水海冰研究的盐偏析模型在咸水中波罗的海冰的生长期间涉及。我们使用了一系列冰盐度曲线和建模的增长率,以检查有效盐分离和增长率之间的关系。结果表明,为盐水海水衍生的型号不适用于波罗的海的咸水水域。我们为冰增长率有效的盐偏析来源的简单模型,适用于各种增长率,在低盐度波罗的海条件下使用和未来波罗的海冰盐度模型的应用。

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