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Pak lodowy

Forma lodu morskiego, który dryfuje i podlega znacznym deformacjom. Jest to lód morski nieprzytwierdzony do brzegu. W Arktyce pak lodowy podlega sezonowym zmianom. Jego zasięg osiąga minimum we wrześniu, po czym wzrasta jesienią i zimą oraz maleje wiosną i latem.

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