2021
DOI: 10.1002/essoar.10509774.1
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Effects of snow and remineralization processes on nutrient distributions in multi-year Antarctic landfast sea ice

Abstract: Antarctic multi-year landfast ice grew upward due to the year-by-year accumulation of snow • Nutrient concentrations decreased in the upper sea ice due to the replacement by clean snow • In deeper sea ice, remineralization by degradation of organic matter drove nutrient concentrations

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