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Arctic Tundra Shifts From Carbon Sink to Source as Permafrost Thaws

A new study reveals over a third of the Arctic-boreal region now emits more carbon than it absorbs, driven by warming temperatures and wildfires.

Overview

  • The Arctic-boreal region, historically a major carbon sink, is now a net emitter of carbon dioxide across 34% of its area, rising to 40% when wildfire emissions are included.
  • Thawing permafrost, which contains vast amounts of stored carbon, is a key driver of this shift, as warming temperatures accelerate decomposition and greenhouse gas release.
  • The study, published in *Nature Climate Change*, combines three decades of satellite and field data from over 200 sites, offering the most comprehensive assessment of the region's carbon flux to date.
  • While some areas are experiencing increased vegetation growth due to longer growing seasons, this 'greening' is insufficient to offset emissions from thawing soils and wildfires.
  • Researchers warn that these changes in the Arctic carbon cycle could significantly impact global climate targets, as permafrost emissions are not always accounted for in national carbon budgets.

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