Literature DB >> 29569788

Large uncertainty in carbon uptake potential of land-based climate-change mitigation efforts.

Andreas Krause1, Thomas A M Pugh1,2, Anita D Bayer1, Wei Li3, Felix Leung4, Alberte Bondeau5, Jonathan C Doelman6, Florian Humpenöder7, Peter Anthoni1, Benjamin L Bodirsky7, Philippe Ciais3, Christoph Müller7, Guillermo Murray-Tortarolo4,8, Stefan Olin9, Alexander Popp7, Stephen Sitch4, Elke Stehfest6, Almut Arneth1.   

Abstract

Most climate mitigation scenarios involve negative emissions, especially those that aim to limit global temperature increase to 2°C or less. However, the carbon uptake potential in land-based climate change mitigation efforts is highly uncertain. Here, we address this uncertainty by using two land-based mitigation scenarios from two land-use models (IMAGE and MAgPIE) as input to four dynamic global vegetation models (DGVMs; LPJ-GUESS, ORCHIDEE, JULES, LPJmL). Each of the four combinations of land-use models and mitigation scenarios aimed for a cumulative carbon uptake of ~130 GtC by the end of the century, achieved either via the cultivation of bioenergy crops combined with carbon capture and storage (BECCS) or avoided deforestation and afforestation (ADAFF). Results suggest large uncertainty in simulated future land demand and carbon uptake rates, depending on the assumptions related to land use and land management in the models. Total cumulative carbon uptake in the DGVMs is highly variable across mitigation scenarios, ranging between 19 and 130 GtC by year 2099. Only one out of the 16 combinations of mitigation scenarios and DGVMs achieves an equivalent or higher carbon uptake than achieved in the land-use models. The large differences in carbon uptake between the DGVMs and their discrepancy against the carbon uptake in IMAGE and MAgPIE are mainly due to different model assumptions regarding bioenergy crop yields and due to the simulation of soil carbon response to land-use change. Differences between land-use models and DGVMs regarding forest biomass and the rate of forest regrowth also have an impact, albeit smaller, on the results. Given the low confidence in simulated carbon uptake for a given land-based mitigation scenario, and that negative emissions simulated by the DGVMs are typically lower than assumed in scenarios consistent with the 2°C target, relying on negative emissions to mitigate climate change is a highly uncertain strategy.
© 2018 John Wiley & Sons Ltd.

Entities:  

Keywords:  BECCS; avoided deforestation and afforestation; carbon dioxide removal; land-based mitigation; negative emissions

Mesh:

Substances:

Year:  2018        PMID: 29569788     DOI: 10.1111/gcb.14144

Source DB:  PubMed          Journal:  Glob Chang Biol        ISSN: 1354-1013            Impact factor:   10.863


  2 in total

1.  Global cooling induced by biophysical effects of bioenergy crop cultivation.

Authors:  Jingmeng Wang; Wei Li; Philippe Ciais; Laurent Z X Li; Jinfeng Chang; Daniel Goll; Thomas Gasser; Xiaomeng Huang; Narayanappa Devaraju; Olivier Boucher
Journal:  Nat Commun       Date:  2021-12-13       Impact factor: 14.919

2.  Land-use emissions play a critical role in land-based mitigation for Paris climate targets.

Authors:  Anna B Harper; Tom Powell; Peter M Cox; Joanna House; Chris Huntingford; Timothy M Lenton; Stephen Sitch; Eleanor Burke; Sarah E Chadburn; William J Collins; Edward Comyn-Platt; Vassilis Daioglou; Jonathan C Doelman; Garry Hayman; Eddy Robertson; Detlef van Vuuren; Andy Wiltshire; Christopher P Webber; Ana Bastos; Lena Boysen; Philippe Ciais; Narayanappa Devaraju; Atul K Jain; Andreas Krause; Ben Poulter; Shijie Shu
Journal:  Nat Commun       Date:  2018-08-07       Impact factor: 14.919

  2 in total

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