Articles | Volume 16, issue 20
https://doi.org/10.5194/bg-16-3977-2019
https://doi.org/10.5194/bg-16-3977-2019
Research article
 | 
17 Oct 2019
Research article |  | 17 Oct 2019

Modelling long-term blanket peatland development in eastern Scotland

Ward Swinnen, Nils Broothaerts, and Gert Verstraeten

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Cited articles

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. 
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.2, 2012. 
Ballantyne, C. K.: After the ice: Holocene geomorphic activity in the Scottish Highlands, Scottish Geogr. J., 124, 8–52, https://doi.org/10.1080/14702540802300167, 2008. 
Ballard, C. E., McIntyre, N., Wheater, H. S., Holden, J., and Wallage, Z. E.: Hydrological modelling of drained blanket peatland, J. Hydrol., 407, 81–93, https://doi.org/10.1016/j.jhydrol.2011.07.005, 2011. 
Beilman, D. W. and Yu, Z.: Differential Response of Peatland Types to Climate: Modeling Peat Accumulation in Continental Western Canada, 38–86, 2001. 
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Short summary
In this study, a new model is presented, which was specifically designed to study the development and carbon storage of blanket peatlands since the last ice age. In the past, two main processes (declining forest cover and rising temperatures) have been proposed as drivers of blanket peatland development on the British Isles. The simulations performed in this study support the temperature hypothesis for the blanket peatlands in the Cairngorms Mountains of central Scotland.
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