Articles | Volume 17, issue 21
https://doi.org/10.5194/bg-17-5285-2020
https://doi.org/10.5194/bg-17-5285-2020
Research article
 | 
05 Nov 2020
Research article |  | 05 Nov 2020

Global peatland area and carbon dynamics from the Last Glacial Maximum to the present – a process-based model investigation

Jurek Müller and Fortunat Joos

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Committed and projected future changes in global peatlands – continued transient model simulations since the Last Glacial Maximum
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Biogeosciences, 18, 3657–3687, https://doi.org/10.5194/bg-18-3657-2021,https://doi.org/10.5194/bg-18-3657-2021, 2021
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Cited articles

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Alexandrov, G. A., Brovkin, V. A., and Kleinen, T.: The influence of climate on peatland extent in Western Siberia since the Last Glacial Maximum, Sci. Rep., 6, 6–11, https://doi.org/10.1038/srep24784, 2016. a
Annan, J. D. and Hargreaves, J. C.: A new global reconstruction of temperature changes at the Last Glacial Maximum, Clim. Past, 9, 367–376, https://doi.org/10.5194/cp-9-367-2013, 2013. a
Baird, A. J., Morris, P. J., and Belyea, L. R.: The DigiBog peatland development model 1: rationale, conceptual model, and hydrological basis, Ecohydrology, 5, 242–255, https://doi.org/10.1002/eco.230, 2012. a
Bartlein, P. J., Harrison, S. P., Brewer, S., Connor, S., Davis, B. A., Gajewski, K., Guiot, J., Harrison-Prentice, T. I., Henderson, A., Peyron, O., Prentice, I. C., Scholze, M., Seppä, H., Shuman, B., Sugita, S., Thompson, R. S., Viau, A. E., Williams, J., and Wu, H.: Pollen-based continental climate reconstructions at 6 and 21 ka: A global synthesis, Clim. Dyn., 37, 775–802, https://doi.org/10.1007/s00382-010-0904-1, 2011. a, b
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We present an in-depth model analysis of transient peatland area and carbon dynamics over the last 22 000 years. Our novel results show that the consideration of both gross positive and negative area changes are necessary to understand the transient evolution of peatlands and their net effect on atmospheric carbon. The study includes the attributions to drivers through factorial simulations, assessments of uncertainty from climate forcing, and determination of the global net carbon balance.
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