Published August 26, 2021 | Version v1
Dataset Open

A biophysical permafrost zonation map in the Northern Hemisphere

  • 1. Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences
  • 2. Alaska Ecoscience
  • 3. Institute of Tibetan Plateau Research, Chinese Academy of Sciences

Description

The biophysical permafrost zonation map was produced using a rule-based GIS model that integrated a new permafrost extent, climate conditions, vegetation structure, soil and topographic conditions, as well as a yedoma map. Different from the previous maps, permafrost in this map is classified into five types: climate-driven, climate-driven/ecosystem-modified, climate-driven/ecosystem protected, ecosystem-driven, and ecosystem-protected.  Excluding glaciers and lakes, the areas of these five types in the Northern Hemisphere are 3.66×106 km2, 8.06×106 km2, 0.62×106 km2, 5.79×106 km2, and 1.63×106 km2, respectively. 81% of the permafrost regions in the Northern Hemisphere are modified, driven, or protected by ecosystems, indicating the dominant role of ecosystems in permafrost stability in the Northern Hemisphere. Permafrost driven solely by climate occupies 19% of permafrost regions, mainly in High Arctic and high mountains areas, such as the Qinghai-Tibet Plateau.

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Additional details

Related works

Is referenced by
Journal article: 10.1088/1748-9326/ac20f3 (DOI)

References

  • Ran Youhua, M. Torre Jorgenson, Li Xin, Jin Huijun, Wu Tonghua, Li Ren, Cheng Guodong. Biophysical permafrost map indicates ecosystem processes dominate permafrost stability in the Northern Hemisphere. Environmental Research Letters. https://doi.org/10.1088/1748-9326/ac20f3, 2021.