Preprints
https://doi.org/10.5194/egusphere-2026-835
https://doi.org/10.5194/egusphere-2026-835
16 Feb 2026
 | 16 Feb 2026
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Quantifying soil organic carbon stocks above the treeline in the Swiss Alps

Michael Zehnder, Annegret Udke, Katrin Meusburger, Frank Hagedorn, Andri Baltensweiler, and Christian Rixen

Abstract. More than 90 % of the total carbon (C) in alpine ecosystems is stored belowground, yet spatial estimates of soil organic carbon (SOC) stocks remain scarce due to limited accessibility and the demanding nature of SOC stock estimates in rocky alpine terrain. By combining new measurements at 144 sites across the Swiss Alps with data from existing inventories, we compiled a comprehensive dataset on SOC stocks totalling 307 sites from treeline to the permafrost region (1750 m – 3100 m a.s.l.). We predicted the spatial distribution of SOC by linking stock measurements to environmental covariates using Quantile Regression Forests (QRF) and produced a SOC stock map at 25 m resolution illustrating the spatial SOC variability in alpine terrain. Our results show that SOC stocks average 7.3 ± 3.3 kg m⁻² in alpine grasslands and 1.8 ± 1.7 kg m⁻² in partly vegetated areas around and above the vegetation line. Overall, the alpine region of Switzerland, which covers one-third of the total country area, stores an estimated amount of 47.6 Mt SOC, representing a non-negligible share of the Swiss greenhouse gas inventory. Vegetation productivity, represented by the Normalized Difference Vegetation Index (NDVI) and topo-climatic covariables, together with vegetation-derived indicators of humus content and soil pH, were highly informative for spatial predictions. This study identifies hotspot regions of SOC storage and influential spatial predictors of its distribution, providing a quantitative baseline for assessing the status-quo and future changes in alpine SOC stocks under continued climate and land-use change. The observed increase in SOC stocks with increasing NDVI suggests that climate change-driven greening at high elevations, where vegetation cover is currently sparse, may enhance SOC storage, although the rates and magnitude of these changes require further investigation.

Competing interests: One of the coauthors, Frank Hagedorn, is a member of the editorial board of Biogeosciences.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
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Michael Zehnder, Annegret Udke, Katrin Meusburger, Frank Hagedorn, Andri Baltensweiler, and Christian Rixen

Status: open (until 03 Apr 2026)

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Michael Zehnder, Annegret Udke, Katrin Meusburger, Frank Hagedorn, Andri Baltensweiler, and Christian Rixen
Michael Zehnder, Annegret Udke, Katrin Meusburger, Frank Hagedorn, Andri Baltensweiler, and Christian Rixen

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Short summary
Most organic carbon in alpine ecosystems is stored belowground, yet its distribution is poorly known. By combining new soil measurements with existing data from across the Swiss Alps, we mapped soil carbon storage from the treeline to permafrost-affected regions. We found that alpine grasslands store large amounts of soil carbon, explained mainly by vegetation productivity, temperature, and terrain. The results provide a baseline to assess how alpine soil carbon may respond to climate change.
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