Seasonality of volcanic eruptions

An analysis of volcanic activity during the last three hundred years reveals that volcanic eruptions exhibit seasonality to a statistically significant degree. This remarkable pattern is observed primarily along the Pacific "Ring of Fire" and locally at some individual volcanoes. Globally,...

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Published in:Journal of Geophysical Research: Solid Earth
Main Authors: Mason, BG, Pyle, D, Dade, W, Jupp, T
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:https://doi.org/10.1029/2002JB002293
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spelling ftuloxford:oai:ora.ox.ac.uk:uuid:65120382-967e-48a7-9e7f-0eb9e48e6560 2023-05-15T16:59:23+02:00 Seasonality of volcanic eruptions Mason, BG Pyle, D Dade, W Jupp, T 2016-07-28 https://doi.org/10.1029/2002JB002293 https://ora.ox.ac.uk/objects/uuid:65120382-967e-48a7-9e7f-0eb9e48e6560 eng eng doi:10.1029/2002JB002293 https://ora.ox.ac.uk/objects/uuid:65120382-967e-48a7-9e7f-0eb9e48e6560 https://doi.org/10.1029/2002JB002293 info:eu-repo/semantics/embargoedAccess Journal article 2016 ftuloxford https://doi.org/10.1029/2002JB002293 2022-06-28T20:14:06Z An analysis of volcanic activity during the last three hundred years reveals that volcanic eruptions exhibit seasonality to a statistically significant degree. This remarkable pattern is observed primarily along the Pacific "Ring of Fire" and locally at some individual volcanoes. Globally, seasonal fluctuations amount to 18% of the historical average monthly eruption rate. In some regions, seasonal fluctuations amount to as much as 50% of the average eruption rate. Seasonality principally reflects the temporal distribution of the smaller, dated eruptions (volcanic explosivity index of 0-2) that dominate the eruption catalog. We suggest that the pattern of seasonality correlates with the annual Earth surface deformation that accompanies the movement of surface water mass during the annual hydrological cycle and illustrate this with respect to global models of surface deformation and regional measurements of annual sea level change. For example, seasonal peaks in the eruption rate of volcanoes in Central America, the Alaskan Peninsula, and Kamchatka coincide with periods of falling regional sea level. In Melanesia, in contrast, peak numbers of volcanic eruptions occur during months of maximal regional sea level and falling regional atmospheric pressure. We suggest that the well-documented slow deformation of Earth's surface that accompanies the annual movements of water mass from oceans to continents acts to impose a fluctuating boundary condition on volcanoes, such that volcanic eruptions tend to be concentrated during periods of local or regional surface change rather than simply being distributed randomly throughout the year. Our findings have important ramifications for volcanic risk assessment and volcanoclimate feedback mechanisms. Copyright 2004 by the American Geophysical Union. Article in Journal/Newspaper Kamchatka ORA - Oxford University Research Archive Pacific Journal of Geophysical Research: Solid Earth 109 B4
institution Open Polar
collection ORA - Oxford University Research Archive
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language English
description An analysis of volcanic activity during the last three hundred years reveals that volcanic eruptions exhibit seasonality to a statistically significant degree. This remarkable pattern is observed primarily along the Pacific "Ring of Fire" and locally at some individual volcanoes. Globally, seasonal fluctuations amount to 18% of the historical average monthly eruption rate. In some regions, seasonal fluctuations amount to as much as 50% of the average eruption rate. Seasonality principally reflects the temporal distribution of the smaller, dated eruptions (volcanic explosivity index of 0-2) that dominate the eruption catalog. We suggest that the pattern of seasonality correlates with the annual Earth surface deformation that accompanies the movement of surface water mass during the annual hydrological cycle and illustrate this with respect to global models of surface deformation and regional measurements of annual sea level change. For example, seasonal peaks in the eruption rate of volcanoes in Central America, the Alaskan Peninsula, and Kamchatka coincide with periods of falling regional sea level. In Melanesia, in contrast, peak numbers of volcanic eruptions occur during months of maximal regional sea level and falling regional atmospheric pressure. We suggest that the well-documented slow deformation of Earth's surface that accompanies the annual movements of water mass from oceans to continents acts to impose a fluctuating boundary condition on volcanoes, such that volcanic eruptions tend to be concentrated during periods of local or regional surface change rather than simply being distributed randomly throughout the year. Our findings have important ramifications for volcanic risk assessment and volcanoclimate feedback mechanisms. Copyright 2004 by the American Geophysical Union.
format Article in Journal/Newspaper
author Mason, BG
Pyle, D
Dade, W
Jupp, T
spellingShingle Mason, BG
Pyle, D
Dade, W
Jupp, T
Seasonality of volcanic eruptions
author_facet Mason, BG
Pyle, D
Dade, W
Jupp, T
author_sort Mason, BG
title Seasonality of volcanic eruptions
title_short Seasonality of volcanic eruptions
title_full Seasonality of volcanic eruptions
title_fullStr Seasonality of volcanic eruptions
title_full_unstemmed Seasonality of volcanic eruptions
title_sort seasonality of volcanic eruptions
publishDate 2016
url https://doi.org/10.1029/2002JB002293
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geographic Pacific
geographic_facet Pacific
genre Kamchatka
genre_facet Kamchatka
op_relation doi:10.1029/2002JB002293
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https://doi.org/10.1029/2002JB002293
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op_doi https://doi.org/10.1029/2002JB002293
container_title Journal of Geophysical Research: Solid Earth
container_volume 109
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