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Health & Science3h 19m ago
A recent study published in Science Advances indicates that permafrost may shift from a carbon sink to a source earlier than expected, around the 2050s, due to the inclusion of previously ignored deep soil carbon in models.
Arctic and northern high latitudes
Who
authors of the new study, researchers, team
What
A recent study published in Science Advances indicates that permafrost may shift from a carbon sink to a source earlier than expected, around the 2050s, due to the inclusion of previously ignored deep soil carbon in models.
When
Mon, 15 Jun 2026 16:59:59 GMT · 3h 19m ago
Where
Arctic and northern high latitudes ·
Why
The Arctic and northern high latitudes are warming about 2–4 times faster than the global average, causing ancient permafrost to thaw and release stored carbon, which, when deep carbon deposits are accounted for, leads to a reversal from a carbon sink to a source.
The Frontline Impact
How this affects you
This recalibration of climate models suggests a more immediate and significant release of greenhouse gases from thawing permafrost than previously understood, demanding urgent attention to the amplified feedback loop contributing to global warming. The inclusion of deep carbon dynamics provides a more accurate picture of future permafrost carbon climate feedbacks.
Story chain
3 events in this thread- Currently Reading3h 19m agoA recent study published in Science Advances indicates that permafrost may shift from a carbon sink to a source earlier than expected, around the 2050s, due to the inclusion of previously ignored deep soil carbon in models.
- Health & Science3h 19m agoNew models including deep soil carbon indicate northern permafrost may shift from a carbon sink to a source around the 2050s, earlier than previous models suggested.Open article
- Health & Science3h 19m agoA new study indicates that northern permafrost may shift from a carbon sink to a carbon source earlier than expected, around the 2050s, due to the inclusion of deep soil carbon in updated models.Open article
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