Evidence map›Paper›PMID 37328462›Full record

ReviewNature communications2023

Continentality determines warming or cooling impact of heavy rainfall events on permafrost.

Alexandra Hamm, Rúna Í Magnússon, Ahmad Jan Khattak, Andrew Frampton

Open access · goldAbstract readReview
In one paragraph

Review in Nature communications, 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 4 papers.

0numbers the graph read from it
0cells of the map it votes in
4citing papers in PubMed
10.0field-weighted citation impact, top 1% of its field
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

4 citing papers in PubMed, 47 citations in OpenAlex.

  1. Article
  2. Article
  3. Article
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4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

4 authors at 3 institutions in 2 countries.

Alexandra HammDepartment of Physical Geography, Stockholm University, Stockholm, Sweden. alexandra.hamm@natgeo.su.se.ORCID http://orcid.org/0000-0003-2785-7672
Rúna Í MagnússonPlant Ecology and Nature Conservation Group, Wageningen University, Wageningen, Netherlands.ORCID http://orcid.org/0000-0003-2254-2612
Ahmad Jan KhattakNOAA Affiliate at Lynker, Office of Water Prediction, National Water Center, Tuscaloosa, AL, USA.
Andrew FramptonDepartment of Physical Geography, Stockholm University, Stockholm, Sweden.ORCID http://orcid.org/0000-0002-4587-6706
Stockholm University · SENOAA National Water CenterWageningen University & Research · NL

Funding

Svenska Forskningsrådet Formas (Swedish Research Council Formas) 2017-00736
6 · The paper itself

Abstract

Permafrost thaw can cause an intensification of climate change through the release of carbon as greenhouse gases. While the effect of air temperature on permafrost thaw is well quantified, the effect of rainfall is highly variable and not well understood. Here, we provide a literature review of studies reporting on effects of rainfall on ground temperatures in permafrost environments and use a numerical model to explore the underlying physical mechanisms under different climatic conditions. Both the evaluated body of literature and the model simulations indicate that continental climates are likely to show a warming of the subsoil and hence increased end of season active layer thickness, while maritime climates tend to respond with a slight cooling effect. This suggests that dry regions with warm summers are prone to more rapid permafrost degradation under increased occurrences of heavy rainfall events in the future, which can potentially accelerate the permafrost carbon feedback.

Indexed as

Greenhouse GasesPermafrostCarbonClimate ChangeCold TemperatureSoilCarbonGreenhouse GasesSoil

Identifiers

PMID37328462
PMCPMC10275877
OpenAlexW4380992806

What OpenQuestion holds

Textmetadata
LicenceCC BY
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.