Abstract
This review deals with properties of sea ice that are relevant to mechanical behavior on a fairly small scale. The main concern is with polycrystalline ice that is more or less intact. This sets the lower limit of scale not far below 0.1 m, and the upper limit around 10 m. However, the discussion is extended to cover the behavior of fragmented ice over broader areas. The latter discussion is intended to bridge the gap between this review, which relates to small-scale natural processes and engineering problems, and companion reviews, which deal with the mechanics of sea ice over very large areas.
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Mellor, M. (1986). Mechanical Behavior of Sea Ice. In: Untersteiner, N. (eds) The Geophysics of Sea Ice. NATO ASI Series. Springer, Boston, MA. https://doi.org/10.1007/978-1-4899-5352-0_3
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