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Soil thawing in Alaska has been accelerating as a result of climate changes, potentially enabling increased carbon dioxide (CO₂) absorption through greater productivity of arctic bramble (Rubus arcticus) plants and other vegetation, but also potentially enabling increased CO₂ output through greater heterotrophic respiration (CO₂ generated by the activity of soil microorganisms). Hydrologist Yonghong Yi and her colleagues developed a model incorporating numerous inputs—years of soil temperature and snow cover data among them—to evaluate the effects of climate changes on the CO₂ balance in Alaska, concluding that net CO₂ is likely to increase if seasonal snow cover arrives earlier relative to the onset of soil surface freezing.