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Ice- and peat-rich permafrost degraded gradually on Eboling Ridge

A snowy alpine landscape at dusk or dawn showing frost-covered coniferous trees densely packed across a frozen plateau under a purple-blue sky.
Research area:Earth and Planetary SciencesClimate change and permafrostPermafrost

What the study found

Ice- and peat-rich permafrost at the EboA observing site on China’s northeastern Qinghai-Tibet Plateau has been degrading gradually. The study reports a slow rise in soil temperature, a small increase in active layer thickness, and some ground settlement linked to melting ground ice.

Why the authors say this matters

The authors say warming climate can accelerate permafrost carbon release and ground ice melt, and they note that the sensitivity of ice- and peat-rich permafrost to climate change had not been quantified. They conclude that the study provides a new understanding of ice-carbon coupling in regulating permafrost changes.

What the researchers tested

The researchers combined observations from the EboA site with the CryoGrid community model to analyze long-term permafrost dynamics from 1941 to 2023. They examined permafrost behavior in ice- and peat-rich ground on the northeastern Qinghai-Tibet Plateau.

What worked and what didn't

The analysis found a soil temperature increase of 0.1°C per 10 years and an active layer increase of 0.03 m per 10 years, with a maximum active layer thickness of 0.88 m. About 19 mm of subsidence occurred due to ground ice melting. The degradation was described as relatively small and slower than in other regions, with organic carbon and high ice content acting as an insulating layer.

What to keep in mind

The abstract does not describe detailed uncertainties, model limitations, or site-to-site comparisons beyond the statement that degradation was slower than in other regions. The findings are specific to the EboA observing site and the period studied.

Key points

  • Permafrost at the EboA site degraded gradually from 1941 to 2023.
  • Soil temperature increased by 0.1°C per 10 years.
  • Active layer thickness increased by 0.03 m per 10 years, reaching a maximum of 0.88 m.
  • About 19 mm of subsidence was linked to ground ice melting.
  • The study says organic carbon and high ice content helped insulate the ground.

Disclosure

Research title:
Ice- and peat-rich permafrost degraded gradually on Eboling Ridge
Authors:
Yuan Huang, Xiaoqing Peng, Oliver W. Frauenfeld, Rong Wang, Hengxing Luo, Chen Yang, Qian Li, Qian Zhao, Panpan Wang, Gubu Qiumo
Institutions:
Lanzhou University, Texas A&M University
Publication date:
2026-03-08
OpenAlex record:
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AI provenance: This post was generated by OpenAI. The original authors did not write or review this post.