Abstract
Forestation is widely proposed for carbon dioxide (CO2) removal, but its impact on climate through changes to atmospheric composition and surface albedo remains relatively unexplored. We assessed these responses using two Earth system models by comparing a scenario with extensive global forest expansion in suitable regions to other plausible futures. We found that forestation increased aerosol scattering and the greenhouse gases methane and ozone following increased biogenic organic emissions. Additionally, forestation decreased surface albedo, which yielded a positive radiative forcing (i.e., warming). This offset up to a third of the negative forcing from the additional CO2 removal under a 4°C warming scenario. However, when forestation was pursued alongside other strategies that achieve the 2°C Paris Agreement target, the offsetting positive forcing was smaller, highlighting the urgency for simultaneous emission reductions.
| Original language | English |
|---|---|
| Pages (from-to) | 860-864 |
| Number of pages | 5 |
| Journal | Science |
| Volume | 383 |
| Issue number | 6685 |
| Early online date | 22 Feb 2024 |
| DOIs | |
| Publication status | Published - 23 Feb 2024 |
Bibliographical note
Publisher Copyright:Copyright © 2024 the authors, some rights reserved;
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 13 Climate Action
ASJC Scopus subject areas
- General
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