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The role of submarine volcanism in atmospheric chemistry

1Citations signalées, ce qui n’est pas une note de qualité
15Institutions déclarées
7Pays d’affiliation déclarés

Rattachement africain : de, fr, nz, gb, be, to, us. Niveau de preuve : code pays fourni par la source.

Le résumé fourni par la source

• CaSO 4 and halogens in the Hunga volcanic cloud were mostly derived from seawater. • Sea salts had a strong influence on the stratospheric volcanic cloud at Hunga. • Small- and large-scale submarine eruptions frequently impact the stratosphere. • Non-submarine eruptions can also inject seawater and sea salts in the stratosphere. Submarine volcanic eruptions can form subaerial plumes that reach the stratosphere. Despite this, the impact of submarine eruptions on climate remains unclear due to a lack of clear geological record, with the recent large-scale Hunga eruption on 15 January 2022 being considered as an isolated case. Here, we review the impact of submarine and subaerial volcanoes in island or coastal settings (i.e., near seawater) on volatile/aerosol loading in the stratosphere. Isotopic δ 34 S signatures of the Hunga ash suggest that CaSO 4 salts on the ash surface are dominantly formed by the evaporation of seawater during the eruption. We infer that SO 2 scavenging on volcanic ash did not play a major role in the lower-than-expected SO 2 detected in the volcanic cloud. Chlorine isotopic compositions (δ 37 Cl) also argue in favor of a seawater-derived origin of the chlorides from ash leachates. Combining petrological, leachate, isotopic and thermal analysis data, we demonstrate a near-absence of halogen degassing from the Hunga magma prior to and during the eruption, and conclude that the chlorine and bromine contents of tropospheric and stratospheric volatile species very dominantly derive from seawater/sea salts. We generalize our findings to all submarine eruptions, and large-scale, non-submarine eruptions in island or coastal settings, and propose that these may commonly form volcanic clouds that incorporate seawater thereby leading to the injection of related components (water vapor, sea salts, halogens) into the stratosphere. This makes seawater inputs a serious consideration when evaluating the long-term impact of volcanoes on climate.

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Le contrôle bibliographique ouvert

DOI retrouvé dans Crossref DOI retrouvé ; titre concordant.

Titre Crossref
The role of submarine volcanism in atmospheric chemistry
Date Crossref
01/12/2025
Éditeur
Elsevier BV
Type
journal-article

Ce recoupement confirme des métadonnées liées au DOI. Il ne confirme ni la méthode ni les conclusions de l’étude, et il ne compte pas comme une seconde source scientifique indépendante.

Les institutions déclarées

Une affiliation ne permet pas de déduire la nationalité d’un auteur.

Les sujets associés

Atmospheric Ozone and ClimateAtmospheric chemistry and aerosolsAtmospheric and Environmental Gas Dynamics

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