B054-07
Global peatland area and carbon dynamics in the near and long term future projected seamlessly from the LGM using a dynamic global vegetation model
Abstract:
Here we present results from the LPX-Bern dynamic global vegetation model. A previously published transient simulation from the LGM to the present[2] serves as the starting point to project into the future. For the slow-reacting system of peatlands, we thus explicitly capture the legacy of the transient evolution over 22,000 years.
For the projections, LPX is forced with climate output from 10 different CMIP6 models, chosen for optimal CMIP6 ensemble representation, and three scenarios ranging from low emission to high emission pathways. Climate is held constant for another 4000 years after 2100 CE or 2300 CE to determine the long term effects of climate change on peatlands. Simulations with constant present climate provide information about already committed changes. Differences between the ensemble members are used to estimate uncertainty. Factorial simulations allow for driver attribution.
With this, we provide an in-depth analysis of possible future global peatland dynamics and estimate the net feedback of these ecosystems.
[1] Gallego-Sala et al. Latitudinal limits to the predicted increase of the peatland carbon sink with warming,Nat. Clim. Change, 8,907-913,2018
[2] Müller, J. & Joos, F. Peatland area and carbon over the past 21 000 years – a global process based model investigation,Biogeosciences Disc.,in review,2020, https://www.biogeosciences-discuss.net/bg-2020-110/