Permafrost Causes Unique Fine-Scale Spatial Variability Across Tundra Soils. Siewert, M. B., Lantuit, H., Richter, A., & Hugelius, G. Global Biogeochemical Cycles, 35(3):e2020GB006659, 2021. _eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GB006659![Permafrost Causes Unique Fine-Scale Spatial Variability Across Tundra Soils [link]](https://bibbase.org/img/filetypes/link.svg "link")
Paper doi abstract bibtex Spatial analysis in earth sciences is often based on the concept of spatial autocorrelation, expressed by W. Tobler as the first law of geography: “everything is related to everything else, but near things are more related than distant things.' Here, we show that subsurface soil properties in permafrost tundra terrain exhibit tremendous spatial variability. We describe the subsurface variability of soil organic carbon (SOC) and ground ice content from the centimeter to the landscape scale in three typical tundra terrain types common across the Arctic region. At the soil pedon scale, that is, from centimeters to 1–2 m, variability is caused by cryoturbation and affected by tussocks, hummocks and nonsorted circles. At the terrain scale, from meters to tens of meters, variability is caused by different generations of ice-wedges. Variability at the landscape scale, that is, ranging hundreds of meters, is associated with geomorphic disturbances and catenary shifts. The co-occurrence and overlap of different processes and landforms creates a spatial structure unique to permafrost environments. The coefficient of variation of SOC at the pedon scale (21%–73%) exceeds that found at terrain (17%–66%) and even landscape scale (24%–67%). Such high values for spatial variation are otherwise found at regional to continental scale. Clearly, permafrost soils do not conform to Tobler's law, but are among the most variable soils on Earth. This needs to be accounted for in mapping and predictions of the permafrost carbon feedbacks through various ecosystem processes. We conclude that scale deserves special attention in permafrost regions.
@article{siewert_permafrost_2021,
title = {Permafrost {Causes} {Unique} {Fine}-{Scale} {Spatial} {Variability} {Across} {Tundra} {Soils}},
volume = {35},
copyright = {© 2021. The Authors.},
issn = {1944-9224},
url = {https://onlinelibrary.wiley.com/doi/abs/10.1029/2020GB006659},
doi = {10.1029/2020GB006659},
abstract = {Spatial analysis in earth sciences is often based on the concept of spatial autocorrelation, expressed by W. Tobler as the first law of geography: “everything is related to everything else, but near things are more related than distant things.' Here, we show that subsurface soil properties in permafrost tundra terrain exhibit tremendous spatial variability. We describe the subsurface variability of soil organic carbon (SOC) and ground ice content from the centimeter to the landscape scale in three typical tundra terrain types common across the Arctic region. At the soil pedon scale, that is, from centimeters to 1–2 m, variability is caused by cryoturbation and affected by tussocks, hummocks and nonsorted circles. At the terrain scale, from meters to tens of meters, variability is caused by different generations of ice-wedges. Variability at the landscape scale, that is, ranging hundreds of meters, is associated with geomorphic disturbances and catenary shifts. The co-occurrence and overlap of different processes and landforms creates a spatial structure unique to permafrost environments. The coefficient of variation of SOC at the pedon scale (21\%–73\%) exceeds that found at terrain (17\%–66\%) and even landscape scale (24\%–67\%). Such high values for spatial variation are otherwise found at regional to continental scale. Clearly, permafrost soils do not conform to Tobler's law, but are among the most variable soils on Earth. This needs to be accounted for in mapping and predictions of the permafrost carbon feedbacks through various ecosystem processes. We conclude that scale deserves special attention in permafrost regions.},
language = {en},
number = {3},
urldate = {2024-03-27},
journal = {Global Biogeochemical Cycles},
author = {Siewert, M. B. and Lantuit, H. and Richter, A. and Hugelius, G.},
year = {2021},
note = {\_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GB006659},
keywords = {\#nosource, ground ice, permafrost, scale, soil organic carbon, tundra soils},
pages = {e2020GB006659},
}
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We describe the subsurface variability of soil organic carbon (SOC) and ground ice content from the centimeter to the landscape scale in three typical tundra terrain types common across the Arctic region. At the soil pedon scale, that is, from centimeters to 1–2 m, variability is caused by cryoturbation and affected by tussocks, hummocks and nonsorted circles. At the terrain scale, from meters to tens of meters, variability is caused by different generations of ice-wedges. Variability at the landscape scale, that is, ranging hundreds of meters, is associated with geomorphic disturbances and catenary shifts. The co-occurrence and overlap of different processes and landforms creates a spatial structure unique to permafrost environments. The coefficient of variation of SOC at the pedon scale (21%–73%) exceeds that found at terrain (17%–66%) and even landscape scale (24%–67%). Such high values for spatial variation are otherwise found at regional to continental scale. Clearly, permafrost soils do not conform to Tobler's law, but are among the most variable soils on Earth. This needs to be accounted for in mapping and predictions of the permafrost carbon feedbacks through various ecosystem processes. 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