Evaluating the terrestrial carbon dioxide removal potential of improved forest management and accelerated forest conversion in Norway. (7th July 2020)

• Record Type: Journal Article
• Authors: Bright, Ryan M.; Allen, Micky; Antón‐Fernández, Clara; Belbo, Helmer; Dalsgaard, Lise; Eisner, Stephanie; Granhus, Aksel; Kjønaas, Olaug J.; Søgaard, Gunnhild; Astrup, Rasmus
• Is Part Of: Global change biology. Volume 26:Number 9(2020)
• Page Start: 5087
• Page End: 5105
• Publication Date: 2020-07-07
• Subjects: afforestation -- climate change mitigation -- land use change -- land‐based mitigation -- low‐productive to high‐productive forest (LtHP) -- reforestation -- surface albedo -- terrestrial ecosystems; Climatic changes -- Environmental aspects -- Periodicals; Troposphere -- Environmental aspects -- Periodicals; Biodiversity conservation -- Periodicals; Eutrophication -- Periodicals; 551.5
• DOI: 10.1111/gcb.15228
• Languages: English
• ISSNs: 1354-1013

Abstract

Abstract: As a carbon dioxide removal measure, the Norwegian government is currently considering a policy of large‐scale planting of spruce ( Picea abies (L) H. Karst) on lands in various states of natural transition to a forest dominated by deciduous broadleaved tree species. Given the aspiration to bring emissions on balance with removals in the latter half of the 21st century in effort to limit the global mean temperature rise to "well below" 2°C, the effectiveness of such a policy is unclear given relatively low spruce growth rates in the region. Further convoluting the picture is the magnitude and relevance of surface albedo changes linked to such projects, which typically counteract the benefits of an enhanced forest CO2 sink in high‐latitude regions. Here, we carry out a rigorous empirically based assessment of the terrestrial carbon dioxide removal (tCDR) potential of large‐scale spruce planting in Norway, taking into account transient developments in both terrestrial carbon sinks and surface albedo over the 21st century and beyond. We find that surface albedo changes would likely play a negligible role in counteracting tCDR, yet given low forest growth rates in the region, notable tCDR benefits from such projects would not be realized until the second half of the 21st century, with maximum benefits occurring even later around 2150. We estimate Norway's total accumulated tCDR potential at 2100 and 2150 (including surface albedo changes) to be 447 (±240) and 852 (±295) Mt CO2 ‐eq. at mean net present values of US$ 12 (±3) and US$ 13 (±2) per ton CDR, respectively. For perspective, the accumulated tCDR potential at 2100 represents around 8 years of Norway's total current annual production‐based (i.e., territorial) CO2 ‐eq. emissions. Abstract : Terrestrial carbon dioxide removal (tCDR) often involves afforestation, although a large potential exists in the way of planting favorable tree species on abandoned lands which have recently or are currently undergoing a process of natural reforestation by pioneering tree species of lower productivity. We estimate such potential in Norway to be −491 Mt CO2 at 2100 although decreases to the surface albedo reduce this amount by 44 Mt CO2 ‐eq. About 76% of this potential (net, including the albedo changes) is due to the conversion of naturally regenerated secondary forests dominated by deciduous broadleaved pioneers to spruce forests of higher productivity.