EGU26-17066, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-17066
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Tuesday, 05 May, 11:35–11:45 (CEST)
 
Room 2.95
A vegetation model based indicator measuring the risk for ecosystem destabilization (EcoRisk)
Fabian Stenzel1,2, Jannes Breier1, Dieter Gerten1,3,4, Sebastian Ostberg1, Sibyll Schaphoff1, and Wolfgang Lucht1,3
Fabian Stenzel et al.
  • 1Potsdam Institute for Climate Impact Research (PIK), Potsdam, Germany (stenzel@pik-potsdam.de)
  • 2Stockholm Resilience Centre, Stockholm University, Stockholm, Sweden
  • 3Department of Geography, Humboldt-Universität zu Berlin, Berlin, Germany
  • 4Integrative Research Institute on Transformations of Human-Environment Systems, Humboldt-Universität zu Berlin, Berlin, Germany

A stable Earth system requires a healthy biosphere, but many ecosystems are being pushed beyond safe limits due to human activities such as land-use, resource extraction and climatic changes.

We map the “risk for ecosystem destabilization” (EcoRisk) due climate and land-use pressures based on simulations with the dynamic global vegetation model LPJmL. EcoRisk quantifies ecosystem dissimilarity relative to a preindustrial reference on a scale ranging from no change (0) to very strong change (1). It captures shifts in the vegetation structure (e.g., transition from forest to savanna), as well as relative (relevant for the local scale) and absolute shifts (relevant for the global scale) in soil and vegetation carbon stocks and fluxes, nitrogen stocks and fluxes, and changes in the water cycle [Stenzel et al. 2024].

Currently, almost 30% of the Earth’s global land area show severe changes (EcoRisk exceeds 0.55, a threshold derived from 10 independent indicators of biosphere integrity). These transgressions have steadily increased since 1600 and accelerated after 1925 [Stenzel et al. 2025]. A preliminary assessment of the future status according to simulations from ISIMIP3b scenarios indicates that EcoRisk continues to rise under SSP3-7.0, whereas under SSP1-2.6 it might plateau after mid-century, depending on the land-use scenario.

EcoRisk however is not only useful as a biosphere integrity indicator, but can also be used for model evaluation, because it can be computed separately for vegetation structure, water, carbon or nitrogen. It thus provides a diagnostic tool for model evaluation, benchmarking, and isolating the sources of change after major code revisions.

Data availability: https://biointegrity.pik-potsdam.de

Stenzel, F.; Braun, J.; Breier, J.; Erb, K.; Gerten, D.; Heinke, J.; Matej, S.; Ostberg, S.; Schaphoff, S. & Lucht, W.: biospheremetrics v1.0.2: an R package to calculate two complementary terrestrial biosphere integrity indicators -- human colonization of the biosphere (BioCol) and risk of ecosystem destabilization (EcoRisk), Geoscientific Model Development, 2024, 17, 3235-3258

Stenzel, F.; Ben Uri, L.; Braun, J.; Breier, J.; Erb, K.; Gerten, D.; Haberl, H.; Matej, S.; Milo, R.; Ostberg, S.; Rockström, J.; Roux, N.; Schaphoff, S. & Lucht, W.: Breaching planetary boundaries: Over half of global land area suffers critical losses in functional biosphere integrity, One Earth, 2025, 8, 101393

How to cite: Stenzel, F., Breier, J., Gerten, D., Ostberg, S., Schaphoff, S., and Lucht, W.: A vegetation model based indicator measuring the risk for ecosystem destabilization (EcoRisk), EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-17066, https://doi.org/10.5194/egusphere-egu26-17066, 2026.