ArticleCommunications earth & environment2023
Joint optimization of land carbon uptake and albedo can help achieve moderate instantaneous and long-term cooling effects.
Article in Communications earth & environment, 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.
What it found
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
The trial behind it
Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.
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Who cites it
6 citing papers in PubMed, 21 citations in OpenAlex.
- Non-Abrupt Vegetation Changes due to Altered Nutrient Balance Make Complex Scale-Dependent Warming and Cooling Effects.Global change biology · 2026Article
- It's cool to be green.Proceedings of the National Academy of Sciences of the United States of America · 2025Article
- Accounting for albedo in carbon market protocols.Nature communications · 2025Article
- Assessing the climate benefits of afforestation in the Canadian Northern Boreal and Southern Arctic.Nature communications · 2025Review
- When and where can coastal wetland restoration increase carbon sequestration as a natural climate solution?Cambridge prisms. Coastal futures · 2024Review
- Joint optimization of land carbon uptake and albedo can help achieve moderate instantaneous and long-term cooling effects.Communications earth & environment · 2023Article
Corrections and comments
PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.
Authors and funding
33 authors at 20 institutions in 14 countries.
Funding
Abstract
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.
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What OpenQuestion holds
Registered trials
Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.