Evidence map›Paper›PMID 37660204›Full record

ArticleScientific reports2023

Atmosphere injection of sea salts during large explosive submarine volcanic eruptions.

M Colombier, I A Ukstins, S Tegtmeier, B Scheu, S J Cronin, S Thivet, J Paredes-Mariño, C Cimarelli, K-U Hess, Taaniela Kula and 2 more

Open access · goldAbstract read
In one paragraph

Article in Scientific reports, 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 2 papers.

0numbers the graph read from it
0cells of the map it votes in
2citing papers in PubMed
2.6field-weighted citation impact, top 11% 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

2 citing papers in PubMed, 12 citations in OpenAlex.

  1. Article
  2. Article
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

12 authors at 5 institutions in 5 countries.

M ColombierDepartment of Earth and Environmental Sciences, Ludwig-Maximilians-Universität München, Munich, Germany. mathieu.colombier@min.uni-muenchen.de.
I A UkstinsSchool of Environment, University of Auckland, Auckland, New Zealand.
S TegtmeierUniversity of Saskatchewan, Institute of Space and Atmospheric Studies, Saskatoon, SK, S7N 5E2, Canada.
B ScheuDepartment of Earth and Environmental Sciences, Ludwig-Maximilians-Universität München, Munich, Germany.
S J CroninSchool of Environment, University of Auckland, Auckland, New Zealand.
S ThivetDepartment of Earth and Environmental Sciences, Ludwig-Maximilians-Universität München, Munich, Germany.
J Paredes-MariñoSchool of Environment, University of Auckland, Auckland, New Zealand.
C CimarelliDepartment of Earth and Environmental Sciences, Ludwig-Maximilians-Universität München, Munich, Germany.
K-U HessDepartment of Earth and Environmental Sciences, Ludwig-Maximilians-Universität München, Munich, Germany.
Taaniela KulaTonga Geological Services, Nuku'alofa, Tonga.
Folauhola H Latu'ilaTonga Geological Services, Nuku'alofa, Tonga.
D B DingwellDepartment of Earth and Environmental Sciences, Ludwig-Maximilians-Universität München, Munich, Germany.
Ludwig-Maximilians-Universität München · DEUniversity of Auckland · NZMinistry of Agriculture and Forestry and Food · TOUniversity of Geneva · CHUniversity of Saskatchewan · CA

Funding

European Research Council ADG 2018 834225
6 · The paper itself

Abstract

The 15 January 2022 submarine eruption at Hunga volcano was the most explosive volcanic eruption in 140 years. It involved exceptional magma and seawater interaction throughout the entire submarine caldera collapse. The submarine volcanic jet breached the sea surface and formed a subaerial eruptive plume that transported volcanic ash, gas, sea salts and seawater up to ~ 57 km, reaching into the mesosphere. We document high concentrations of sea salts in tephra (volcanic ash) collected shortly after deposition. We also discuss the potential climatic consequences of large-scale injection of salts into the upper atmosphere during submarine eruptions. Sodium chloride in these volcanic plumes can reach extreme concentrations, and dehalogenation of chlorides and bromides poses the risk of long-term atmospheric and weather impact. Salt content in rapidly collected tephra samples may also be used as a proxy to estimate the water:magma ratio during eruption, with implications for quantification of fragmentation efficiency in submarine breaching events. The balance between salt loading into the atmosphere versus deposition in ash aggregates is a key factor in understanding the atmospheric and climatic consequences of submarine eruptions.

Identifiers

PMID37660204
PMCPMC10475066
OpenAlexW4386387583

What OpenQuestion holds

Textmetadata
LicenceCC BY
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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.