Soil organic carbon stocks in a mountain permafrost area with extensive solifluction (Disko Island, west Greenland)

This study presents a detailed soil organic carbon (SOC) inventory for the Blæsedalen catchment, Disko Island. The study area has a mountainous setting (sea level to c. 800-m elevation), largely dominated by continuous permafrost. A total of twenty-eight soil profiles were sampled, with additional plant cover observations at eighteen sites. The landscape-level mean SOC 0- to 100-cm storage based on land cover upscaling is 4.07 ± 0.74 kg C m−2. These stocks are largely found in the vegetated zone below 400-m elevation. Due to generally deep active layers, only about 4 percent of the total SOC stock is stored in the permafrost layer. An additional upscaling using landform criteria results in a mean stock of 4.01 ± 1.21 kg C m−2. A prominent landform class is “solifluction areas,” which occupies 18 percent of the total study area but represents 56 percent of the total SOC stock. This class has a highly variable SOC 0- to 100-cm stock (0.86–25.5 kg C m−2), but the mean of 12.6 kg C m−2 is much higher than the landscape average. Both landscape-level mean SOC 0- to 100-cm stock estimates in this study are similar, but land cover provides more constrained SOC ranges than landform upscaling.

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Publication Details

Journal
Arctic Antarctic and Alpine Research
Published
2026-04-01
DOI
https://doi.org/10.1080/15230430.2026.2627688
Primary Topic
Climate change and permafrost
Type
article
Field-Weighted Citation Impact
0.00

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article

Soil organic carbon stocks in a mountain permafrost area with extensive solifluction (Disko Island, west Greenland)

Peter Kuhry, Eirini Makopoulou
Arctic Antarctic and Alpine Research
Climate change and permafrost
article

Soil organic carbon stocks in a mountain permafrost area with extensive solifluction (Disko Island, west Greenland)

Peter Kuhry, Eirini Makopoulou
article en

Abstract

This study presents a detailed soil organic carbon (SOC) inventory for the Blæsedalen catchment, Disko Island. The study area has a mountainous setting (sea level to c. 800-m elevation), largely dominated by continuous permafrost. A total of twenty-eight soil profiles were sampled, with additional plant cover observations at eighteen sites. The landscape-level mean SOC 0- to 100-cm storage based on land cover upscaling is 4.07 ± 0.74 kg C m−2. These stocks are largely found in the vegetated zone below 400-m elevation. Due to generally deep active layers, only about 4 percent of the total SOC stock is stored in the permafrost layer. An additional upscaling using landform criteria results in a mean stock of 4.01 ± 1.21 kg C m−2. A prominent landform class is “solifluction areas,” which occupies 18 percent of the total study area but represents 56 percent of the total SOC stock. This class has a highly variable SOC 0- to 100-cm stock (0.86–25.5 kg C m−2), but the mean of 12.6 kg C m−2 is much higher than the landscape average. Both landscape-level mean SOC 0- to 100-cm stock estimates in this study are similar, but land cover provides more constrained SOC ranges than landform upscaling.

Arctic Antarctic and Alpine ResearchVol. 58(1)
Stockholm University (SE)
NordForsk
Life in Land
Openalex Percentile: Top 24%
Climate change and permafrost
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