Anders Lindroth
Professor
Joint optimization of land carbon uptake and albedo can help achieve moderate instantaneous and long-term cooling effects
Author
Summary, in English
Both carbon dioxide uptake and albedo of the land surface affect global climate. However, climate change mitigation by increasing carbon uptake can cause a warming trade-off by decreasing albedo, with most research focusing on afforestation and its interaction with snow. Here, we present carbon uptake and albedo observations from 176 globally distributed flux stations. We demonstrate a gradual decline in maximum achievable annual albedo as carbon uptake increases, even within subgroups of non-forest and snow-free ecosystems. Based on a paired-site permutation approach, we quantify the likely impact of land use on carbon uptake and albedo. Shifting to the maximum attainable carbon uptake at each site would likely cause moderate net global warming for the first approximately 20 years, followed by a strong cooling effect. A balanced policy co-optimizing carbon uptake and albedo is possible that avoids warming on any timescale, but results in a weaker long-term cooling effect.
Department/s
- Dept of Physical Geography and Ecosystem Science
- BECC: Biodiversity and Ecosystem services in a Changing Climate
Publishing year
2023-12
Language
English
Publication/Series
Communications Earth and Environment
Volume
4
Issue
1
Document type
Journal article
Publisher
Springer Nature
Topic
- Climate Research
Status
Published
ISBN/ISSN/Other
- ISSN: 2662-4435