Preprints
https://doi.org/10.5194/egusphere-2026-4735
https://doi.org/10.5194/egusphere-2026-4735
09 Sep 2026
 | 09 Sep 2026
Status: this preprint is open for discussion and under review for SOIL (SOIL).

From in situ to remote sensing: a framework for quantifying boundary-condition sensitivity in soil organic carbon models across diverse European sites

Yue Zhou, Maria Costanza Andrenelli, Quentin Beauclaire, Eyal Ben-Dor, Sara Bergante, Javier Bravo-García, David de la Fuente Blanco, Asa Gholizadeh, David Čejka, Sabine Chabrillat, Bernard Heinesch, Laura Hernandez Mateo, Kevin Kuehl, Bernard Longdoz, Carlos Lozano Fondón, Petr Maca, Robert Milewski, Stefano Monaco, Dimitra Palantza, Francesco Palazzi, Maria Fantappiè, Roberta Farina, Marmar Sabetizadeh, Benjamin Sanchez, Inés Santín, Jonti Evan Shepherd, Judit Torres, Marta Gómez-Giménez, Bas van Wesemael, and Bertrand Guenet

Abstract. Process-based soil organic carbon (SOC) models are widely used for carbon accounting and assessments. For applications beyond experimental sites, remote sensing–derived inputs are often used to complement or replace in situ boundary conditions. This substitution introduces additional sensitivity that has rarely been explicitly quantified. Here, we propose a general framework to quantify boundary-condition sensitivity in SOC modelling, distinguishing between dynamic sensitivity, which reflects deviations in the temporal trajectory of SOC stocks, and endpoint sensitivity, which captures differences in estimated SOC changes over defined reporting periods. Sensitivity is quantified by comparing substitution simulations, in which boundary conditions are replaced one by one with remote sensing–derived spatial datasets, against a baseline simulation driven by in situ observations. The framework is applied to 16 long-term experimental sites across Europe, covering diverse land-use types and environmental conditions.

Boundary-condition substitution affected both SOC trajectories and endpoint estimates, although the magnitude and form of these effects varied among inputs. Initial SOC, vegetation-derived carbon inputs, and climate data were the dominant drivers of dynamic sensitivity. Fixed endpoint sensitivity was generally small relative to measured SOC changes, supporting the use of remote sensing–derived spatial datasets as scalable boundary-condition proxies for SOC modelling. Rolling endpoint sensitivity further revealed that SOC change assessments depend not only on SOC dynamics but also on the selected reporting window. Short reporting periods were more affected by short-term variability, whereas longer periods were more susceptible to accumulated deviations. A reporting window of approximately 15–30 years provided a practical balance between these effects.

Overall, the framework enables a systematic quantification of sensitivity arising from boundary-condition substitution, enabling evaluation of both trajectory and reporting robustness. These findings highlight the importance of jointly considering critical boundary conditions and reporting-window design when applying remote sensing–driven SOC modelling for regional carbon accounting.

Competing interests: At least one of the (co-)authors is a member of the editorial board of SOIL.

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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Yue Zhou, Maria Costanza Andrenelli, Quentin Beauclaire, Eyal Ben-Dor, Sara Bergante, Javier Bravo-García, David de la Fuente Blanco, Asa Gholizadeh, David Čejka, Sabine Chabrillat, Bernard Heinesch, Laura Hernandez Mateo, Kevin Kuehl, Bernard Longdoz, Carlos Lozano Fondón, Petr Maca, Robert Milewski, Stefano Monaco, Dimitra Palantza, Francesco Palazzi, Maria Fantappiè, Roberta Farina, Marmar Sabetizadeh, Benjamin Sanchez, Inés Santín, Jonti Evan Shepherd, Judit Torres, Marta Gómez-Giménez, Bas van Wesemael, and Bertrand Guenet

Status: open (until 21 Oct 2026)

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Yue Zhou, Maria Costanza Andrenelli, Quentin Beauclaire, Eyal Ben-Dor, Sara Bergante, Javier Bravo-García, David de la Fuente Blanco, Asa Gholizadeh, David Čejka, Sabine Chabrillat, Bernard Heinesch, Laura Hernandez Mateo, Kevin Kuehl, Bernard Longdoz, Carlos Lozano Fondón, Petr Maca, Robert Milewski, Stefano Monaco, Dimitra Palantza, Francesco Palazzi, Maria Fantappiè, Roberta Farina, Marmar Sabetizadeh, Benjamin Sanchez, Inés Santín, Jonti Evan Shepherd, Judit Torres, Marta Gómez-Giménez, Bas van Wesemael, and Bertrand Guenet
Yue Zhou, Maria Costanza Andrenelli, Quentin Beauclaire, Eyal Ben-Dor, Sara Bergante, Javier Bravo-García, David de la Fuente Blanco, Asa Gholizadeh, David Čejka, Sabine Chabrillat, Bernard Heinesch, Laura Hernandez Mateo, Kevin Kuehl, Bernard Longdoz, Carlos Lozano Fondón, Petr Maca, Robert Milewski, Stefano Monaco, Dimitra Palantza, Francesco Palazzi, Maria Fantappiè, Roberta Farina, Marmar Sabetizadeh, Benjamin Sanchez, Inés Santín, Jonti Evan Shepherd, Judit Torres, Marta Gómez-Giménez, Bas van Wesemael, and Bertrand Guenet
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Short summary
Modelling changes in soil carbon stocks often relies on field measurements, such as temperature, rainfall and plant growth, but these data are not widely available across large areas. Using 16 long-term experiments data across Europe, we tested how model results changed when field measurements were replaced with satellite-based and other spatial data. Overall, spatial data produced reliable estimates of soil carbon change, supporting their use in large-scale assessments.
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