Impact of Volcanic Eruptions on the Atmosphere

A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Air Quality".

Deadline for manuscript submissions: closed (30 April 2024) | Viewed by 1919

Special Issue Editors


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Guest Editor
Istituto Nazionale di Geofisica e Vulcanologia, 90146 Palermo, Italy
Interests: geochemistry; stable isotopes in CO2; volcanic gases; gas hazard; GIS; gas emissions in urban zones; aqueous geochemistry; environmental geochemistry
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Guest Editor
Dipartimento di Scienze della Terra e del Mare, Università degli Studi di Palermo, Via Archirafi, 36, 90123 Palermo, Italy
Interests: geochemistry and volcanology; environmental impact of volcanic activity

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Guest Editor
Dipartimento di Scienze della Terra e del Mare, Università degli Studi di Palermo, Via Archirafi, 36, 90123 Palermo, Italy
Interests: trace element geochemistry; volcanic emissions; volcanic particulate; passive degassing volcanoes; volcanic ashes; atmospheric deposition; environmental impact of volcanoes; active and passive biomonitoring

Special Issue Information

Dear Colleagues,

The impact of volcanic eruptions on the atmosphere is a matter of great interest to scientists and researchers worldwide. Volcanic activity releases a vast amount of gas, ash, and aerosols that can have a significant impact on our planet’s climate and air quality. These eruptions can inject large amounts of carbon dioxide (CO2), sulfur dioxide (SO2) and other gases into the stratosphere, where they can persist for years and have long-lasting effects. For example, sulfur dioxide reacts with water vapor, forming sulfuric acid aerosols that can scatter and absorb solar radiation, leading to a cooling effect on the Earth's surface. Volcanic eruptions can also have detrimental effects on air quality. Fine ash particles and aerosols can have health impacts on local populations, leading to respiratory issues and other ailments.

Considering the importance of understanding the impact of volcanic eruptions on the atmosphere, we invite researchers and scientists to submit papers for a Special Issue on this subject. This Special Issue aims to gather cutting-edge research, observations, and modelling studies to enhance our knowledge of how volcanic eruptions influence our atmosphere. We encourage the submission of papers focusing on a range of topics, such as the climate effects of volcanic emissions, the impact on atmospheric depositions and related atmospheric chemical processes, ash dispersion modelling and how it can influence the geochemical cycle of the elements, the impact of air quality on health and the environment, and mitigation strategies.

The objective of this Special Issue is to provide a comprehensive overview of the current state of knowledge and foster further advancements in this critical field. Contributions from interdisciplinary research teams, incorporating geology, atmospheric science, remote sensing, environmental geochemistry, and health sciences, among others, are highly encouraged.

Dr. Roberto M.R. Di Martino
Prof. Dr. Francesco Parello
Dr. Sergio Calabrese
Guest Editors

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Keywords

  • geochemistry
  • volcanic eruptions
  • atmosphere
  • volcanic gases
  • aerosols
  • volcanic ashes
  • air quality
  • gas hazard
  • atmospheric deposition
  • human health

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Published Papers (2 papers)

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Research

10 pages, 1781 KiB  
Article
Exposure to Acid Aerosols in the Visiting Areas of the Poás Volcano National Park, Costa Rica
by Christian Vargas Jiménez, José Pablo Sibaja Brenes, Rosa Alfaro Solís, Henry Borbón Alpízar, Mónica Brenes Ortiz and Maricruz Arguedas González
Atmosphere 2024, 15(7), 848; https://doi.org/10.3390/atmos15070848 - 19 Jul 2024
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Abstract
Poás Volcano made a magmatic eruption in April 2017. The volcanic outburst resulted in an ash and vapor column towering over three kilometers high. Since that time, there has been a continual release of gases, aerosols, and more recently, ash, posing potential issues [...] Read more.
Poás Volcano made a magmatic eruption in April 2017. The volcanic outburst resulted in an ash and vapor column towering over three kilometers high. Since that time, there has been a continual release of gases, aerosols, and more recently, ash, posing potential issues for visitors and park rangers. In this work, the potential for exposure to acid gases and aerosols faced by park rangers, officials, and visitors to the Poás Volcano National Park was evaluated, and the concentrations found were compared with the exposure limits established by the Occupational Safety and Health Administration (OSHA). The study was conducted between October 2021 and November 2022. the concentrations of HCl(g), HNO3(ac), HF(g), and H2SO4(ac) were determined at three strategic points: the ranger station, the visitor center, and the main crater viewpoint. The maximum concentrations obtained were (7.0 ± 1.6) ppb for HCl(g), (6.2 ± 2.8) ppb for HNO3(ac), and (0.029 ± 0.044) ppm for H2SO4(ac). There were no concentration values above the detection limit (0.94 μg/m3) for HF(g). By comparing the data obtained with similar studies, it is concluded that the measured values in Poás Volcano National Park are low and only show similarities to the results found in volcanoes within the national territory. The exposure limit established by OSHA (0.02 ppm) was only surpassed by H2SO4(ac), and could be the cause of health effects experienced over the years by park rangers. To minimize these risks, the use of personal protective equipment and air quality monitoring is essential. Full article
(This article belongs to the Special Issue Impact of Volcanic Eruptions on the Atmosphere)
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10 pages, 1124 KiB  
Article
Five Large 13th Century C.E. Volcanic Eruptions Recorded in Antarctica Ice Cores
by Jihong Cole-Dai, Derek L. Brandis and Dave G. Ferris
Atmosphere 2024, 15(6), 661; https://doi.org/10.3390/atmos15060661 - 30 May 2024
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Abstract
Major explosive volcanic eruptions impact the climate by altering the radiative balance of the atmosphere and through feedback mechanisms in the climate system. The extent of the impact depends on the magnitude (aerosol mass loading) and the number or frequency of such eruptions. [...] Read more.
Major explosive volcanic eruptions impact the climate by altering the radiative balance of the atmosphere and through feedback mechanisms in the climate system. The extent of the impact depends on the magnitude (aerosol mass loading) and the number or frequency of such eruptions. Multiple Antarctica ice core records of past volcanic eruptions reveal that the number (5) of major eruptions (volcanic sulfate deposition flux greater than 10 kg km−2) was the highest in the 13th century over the last two millennia. Signals of four of the five eruptions are dated to the second half of the century, indicating consecutive major eruptions capable of causing sustained climate impact via known feedback processes. The fact that signals of four corresponding eruptions have been found in a Greenland ice core indicates that four of the five 13th century eruptions were probably by volcanoes in the low latitudes (between 20° N and 20° S) with substantial aerosol mass loading. These eruptions in the low latitudes likely exerted the strongest volcanic impact on climate in the last two millennia. Full article
(This article belongs to the Special Issue Impact of Volcanic Eruptions on the Atmosphere)
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