ArticleScience advances2022
Northern Hemisphere vegetation change drives a Holocene thermal maximum.
Article in Science advances, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 7 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.
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Who cites it
7 citing papers in PubMed.
- The seasonal temperature conundrum for the Holocene.Science advances · 2025Article
- Assessing the climate benefits of afforestation in the Canadian Northern Boreal and Southern Arctic.Nature communications · 2025Review
- Tropical Andean climate variations since the last deglaciation.Proceedings of the National Academy of Sciences of the United States of America · 2024Article
- Spatial patterns of Holocene temperature changes over mid-latitude Eurasia.Nature communications · 2024Article
- Delayed postglacial colonization ofeLife · 2023Article
- Review
- The Holocene temperature conundrum answered by mollusk records from East Asia.Nature communications · 2022Article
Corrections and comments
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Authors and funding
5 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The Holocene thermal maximum, a period of global warmth evident in early to mid-Holocene proxy reconstructions, is controversial. Most model simulations of the Holocene have not reproduced this warming, leading to a disagreement known as the Holocene Temperature Conundrum. Pollen records document the expansion of vegetation in the early and mid-Holocene African Sahara and Northern Hemisphere mid- and high latitudes, which has been overlooked in previous modeling studies. Here, we use time slice simulations of the Community Earth System Model to assess the impact of Northern Hemisphere vegetation change on Holocene annual mean temperatures. Our simulations indicate that expansion of Northern Hemisphere vegetation 9000 and 6000 years ago warms Earth's surface by ~0.8° and 0.7°C, respectively, producing a better match with proxy-based reconstructions. Our results suggest that vegetation change is critical for modeling Holocene temperature evolution and highlight its role in driving a mid-Holocene temperature maximum.
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Registered trials
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