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For the first time an attempt is made to derive a theoretical relationship between sea‐ice strength and the controlling factors of salinity, temperature, and density. A geometric model of the ice‐brine relationship is constructed from photographs and used to calculate tensile strength of warm (above −20°C) sea ice. The theoretical results compare well with experimental data. The model developed can be extended to colder temperatures by considering the effect of solid salts.
Anderson et al. (Fri,) studied this question.
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