Evidence map›Paper›PMID 39738082›Full record

ArticleNature communications2024

Future increase in compound soil drought-heat extremes exacerbated by vegetation greening.

Jun Li, Yao Zhang, Emanuele Bevacqua, Jakob Zscheischler, Trevor F Keenan, Xu Lian, Sha Zhou, Hongying Zhang, Mingzhu He, Shilong Piao

Erratum issuedAbstract read
In one paragraph

Article in Nature communications, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. An erratum has been issued. Cited by 12 papers.

0numbers the graph read from it
0cells of the map it votes in
12citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

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.

2 · The registry

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.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

12 citing papers in PubMed.

  1. Increasing risk of vapor pressure deficit exceeding critical thresholds for tree growth.Proceedings of the National Academy of Sciences of the United States of America · 2026
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  3. A potential overestimation of COProceedings of the National Academy of Sciences of the United States of America · 2026
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4 · The record

Corrections and comments

5 · Who and what money

Authors and funding

10 authors.

Jun LiInstitute of Carbon Neutrality, Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China.ORCID 0000-0003-1412-5261
Yao ZhangInstitute of Carbon Neutrality, Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China. zhangyao@pku.edu.cn.ORCID 0000-0002-7468-2409
Emanuele BevacquaDepartment of Compound Environmental Risks, Helmholtz Centre for Environmental Research-UFZ, Leipzig, Germany.ORCID 0000-0003-0472-5183
Jakob ZscheischlerDepartment of Compound Environmental Risks, Helmholtz Centre for Environmental Research-UFZ, Leipzig, Germany.ORCID 0000-0001-6045-1629
Trevor F KeenanEarth and Environmental Sciences Area, Lawrence Berkeley National Laboratory, Berkeley, CA, USA.ORCID 0000-0002-3347-0258
Xu LianDepartment of Earth and Environmental Engineering, Columbia University, New York, NY, USA.ORCID 0000-0002-1428-3529
Sha ZhouState Key Laboratory of Earth Surface Processes and Resources Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing, China.ORCID 0000-0001-7161-5959
Hongying ZhangInstitute of Carbon Neutrality, Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China.
Mingzhu HeInstitute of Carbon Neutrality, Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China.
Shilong PiaoInstitute of Carbon Neutrality, Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China.ORCID 0000-0001-8057-2292

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Compound soil drought and heat extremes are expected to occur more frequently with global warming, causing wide-ranging socio-ecological repercussions. Vegetation modulates air temperature and soil moisture through biophysical processes, thereby influencing the occurrence of such extremes. Global vegetation cover is broadly expected to increase under climate change, but it remains unclear whether vegetation greening will alleviate or aggravate future increases in compound soil drought-heat events. Here, using a suite of state-of-the-art model simulations, we show that the projected vegetation greening will increase the frequency of global compound soil drought-heat events, equivalent to 12-21% of the total increment at the end of 21st century. This increase is predominantly driven by reduced albedo and enhanced transpiration associated with increased leaf area. Although greening-induced transpiration enhancement has counteracting cooling and drying effects, the excessive water loss in the early growing season can lead to later soil moisture deficits, amplifying compound soil drought-heat extremes during the subsequent warm season. These changes are most pronounced in northern high latitudes and are dominated by the warming effect of CO

Indexed as

Climate ChangeDroughtsHot TemperatureSoilCarbon DioxideGlobal WarmingPlant LeavesPlant TranspirationSeasonsWaterCarbon DioxideSoilWater

Identifiers

PMID39738082
PMCPMC11686399

What OpenQuestion holds

Textmetadata
LicenceCC BY-NC-ND
Read underepoch 390

Registered trials

None linked

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.