Limited Mitigation Potential of Forestation Under a High Emissions Scenario: Results From Multi‐Model and Single Model Ensembles

Author:

Loughran Tammas F.1ORCID,Ziehn Tilo1ORCID,Law Rachel1ORCID,Canadell Josep G.2ORCID,Pongratz Julia34ORCID,Liddicoat Spencer5ORCID,Hajima Tomohiro6ORCID,Ito Akihiko7ORCID,Lawrence David M.8ORCID,Arora Vivek K.9ORCID

Affiliation:

1. CSIRO Environment Aspendale VIC Australia

2. CSIRO Environment Canberra ACT Australia

3. Ludwig‐Maximilians‐Universität München Munich Germany

4. Max Planck Institute for Meteorology Hamburg Germany

5. Met Office Hadley Centre Exeter UK

6. Research Institute for Global Change Japan Agency for Marine‐Earth Science and Technology Kanagawa Japan

7. National Institute for Environmental Studies Tsukuba Japan

8. Climate and Global Dynamics Laboratory National Center for Atmospheric Research Boulder CO USA

9. Canadian Centre for Climate Modelling and Analysis, Environment and Climate Change Canada University of Victoria Victoria BC Canada

Abstract

AbstractForestation is a major component of future long‐term emissions reduction and CO2 removal strategies, but the viability of carbon stored in vegetation under future climates is highly uncertain. We analyze the results from seven CMIP6 models for a combined scenario with high fossil fuel emissions (from SSP5‐8.5) and forest expansion (from SSP1‐2.6) which has ∼4.8% increase in global total forest cover relative to 2015. This scenario aims to demonstrate the ability of forestation strategies to mitigate climate change under continued increasing CO2 emissions and includes the potential impacts of increased CO2 concentration and a warming climate on vegetation growth. The model intercomparison shows that forestation as a CO2 removal strategy has limited impact on global climate under a high global warming scenario, despite generating a substantial cumulative carbon sink of 10–60 Pg C over the period 2015–2100. Using a single model ensemble, we show that there are local increases in warm extremes in response to forestation associated with decreases in the number of cool days. Furthermore, we find evidence of a shift in the global carbon balance, whereby increased carbon storage on land of ∼25 Pg C by 2100 associated with forestation has a concomitant decrease in the carbon uptake by the ocean due to reduced atmospheric CO2 concentrations.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry

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