Articles | Volume 16, issue 7
https://doi.org/10.5194/gmd-16-2011-2023
https://doi.org/10.5194/gmd-16-2011-2023
Model description paper
 | 
13 Apr 2023
Model description paper |  | 13 Apr 2023

The Permafrost and Organic LayEr module for Forest Models (POLE-FM) 1.0

Winslow D. Hansen, Adrianna Foster, Benjamin Gaglioti, Rupert Seidl, and Werner Rammer

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Cited articles

Abbott, B. W. and Jones, J. B.: Permafrost collapse alters soil carbon stocks, respiration, CH4, and N2O in upland tundra, Glob.Change Biol., 21, 4570–4587, https://doi.org/10.1111/gcb.13069, 2015. 
Albrich, K., Rammer, W., Turner, M. G., Ratajczak, Z., Braziunas, K. H., Hansen, W. D., and Seidl, R.: Simulating forest resilience: A review, Global Ecol. Biogeogr., 29, 2082–2096, https://doi.org/10.1111/geb.13197, 2020. 
Alexander, H. D. and Mack, M. C.: A canopy shift in interior Alaskan boreal forests: Consequences for above- and belowground carbon and nitrogen pools during post-fire succession, Ecosystems, 19, 98–114, https://doi.org/10.1007/s10021-015-9920-7, 2016. 
Anderegg, W. R. L., Wu, C., Acil, N., Carvalhais, N., Pugh, T. A. M., Sadler, J. P., and Seidl, R.: A climate risk analysis of Earth's forests in the 21st century, Science, 377, 1099–1103, https://doi.org/10.1126/science.abp9723, 2022. 
Anderson, P. M., Edwards, M. E., and Brubaker, L. B.: Results and paleoclimate implications of 35 years of paleoecological research in Alaska, in: Developments in Quaternary Sciences, vol. 1, Elsevier, 427–440, https://doi.org/10.1016/S1571-0866(03)01019-4, 2003. 
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Short summary
Permafrost and the thick soil-surface organic layers that insulate permafrost are important controls of boreal forest dynamics and carbon cycling. However, both are rarely included in process-based vegetation models used to simulate future ecosystem trajectories. To address this challenge, we developed a computationally efficient permafrost and soil organic layer module that operates at fine spatial (1 ha) and temporal (daily) resolutions.
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