Seismogenic-Triggering Mechanism of Gas Emission Activizations on the Arctic Shelf and Associated Phases of Abrupt Warming

A seismogenic trigger mechanism is proposed to explain the abrupt climate warming phases in the Arctic as a result of strong mechanical disturbances in the marginal region of the Arctic lithosphere. Those disturbances might have been caused by great earthquakes in the Aleutian subduction zone, and s...

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Published in:Geosciences
Main Author: Leopold Lobkovsky
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2020
Subjects:
Ice
Online Access:https://doi.org/10.3390/geosciences10110428
https://doaj.org/article/0af00fe100484431bec44fe53c83c530
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spelling ftdoajarticles:oai:doaj.org/article:0af00fe100484431bec44fe53c83c530 2023-05-15T13:14:45+02:00 Seismogenic-Triggering Mechanism of Gas Emission Activizations on the Arctic Shelf and Associated Phases of Abrupt Warming Leopold Lobkovsky 2020-10-01T00:00:00Z https://doi.org/10.3390/geosciences10110428 https://doaj.org/article/0af00fe100484431bec44fe53c83c530 EN eng MDPI AG https://www.mdpi.com/2076-3263/10/11/428 https://doaj.org/toc/2076-3263 doi:10.3390/geosciences10110428 2076-3263 https://doaj.org/article/0af00fe100484431bec44fe53c83c530 Geosciences, Vol 10, Iss 428, p 428 (2020) abrupt climate warming Arctic great earthquakes Aleutian subduction zone tectonic waves trigger mechanism Geology QE1-996.5 article 2020 ftdoajarticles https://doi.org/10.3390/geosciences10110428 2022-12-31T05:03:38Z A seismogenic trigger mechanism is proposed to explain the abrupt climate warming phases in the Arctic as a result of strong mechanical disturbances in the marginal region of the Arctic lithosphere. Those disturbances might have been caused by great earthquakes in the Aleutian subduction zone, and slowly propagated across the Arctic shelf and adjacent regions, triggering the methane release from permafrost and metastable gas hydrates, followed by greenhouse gas emissions into the atmosphere. The proposed mechanism is based on the identified correlation between the series of the great earthquakes in the Aleutian island arc, which occurred in the early and middle of the 20th century, and the two phases of sharp climate warming, which began in 1920 and 1980. There is a 20-year time lag between these events, which is explained by the time of arrival of deformation waves in the lithosphere (propagating with a velocity of about 100 km per year) at the Arctic shelf and adjacent land from the Aleutian subduction zone, the region of their generation. The trigger mechanism causing the methane release from permafrost and metastable gas hydrates is related to the destruction of micro-sized ice films covering gas hydrate particles, the elements highly important for hydrate self-preservation, as well as destruction of gas-saturated micropores in permafrost rocks due to the slight additional stresses associated with deformation waves, and thus emergence of conditions favorable for gas filtration and its subsequent emission. Article in Journal/Newspaper Aleutian Island Arctic Ice permafrost Directory of Open Access Journals: DOAJ Articles Arctic Geosciences 10 11 428
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic abrupt climate warming
Arctic
great earthquakes
Aleutian subduction zone
tectonic waves
trigger mechanism
Geology
QE1-996.5
spellingShingle abrupt climate warming
Arctic
great earthquakes
Aleutian subduction zone
tectonic waves
trigger mechanism
Geology
QE1-996.5
Leopold Lobkovsky
Seismogenic-Triggering Mechanism of Gas Emission Activizations on the Arctic Shelf and Associated Phases of Abrupt Warming
topic_facet abrupt climate warming
Arctic
great earthquakes
Aleutian subduction zone
tectonic waves
trigger mechanism
Geology
QE1-996.5
description A seismogenic trigger mechanism is proposed to explain the abrupt climate warming phases in the Arctic as a result of strong mechanical disturbances in the marginal region of the Arctic lithosphere. Those disturbances might have been caused by great earthquakes in the Aleutian subduction zone, and slowly propagated across the Arctic shelf and adjacent regions, triggering the methane release from permafrost and metastable gas hydrates, followed by greenhouse gas emissions into the atmosphere. The proposed mechanism is based on the identified correlation between the series of the great earthquakes in the Aleutian island arc, which occurred in the early and middle of the 20th century, and the two phases of sharp climate warming, which began in 1920 and 1980. There is a 20-year time lag between these events, which is explained by the time of arrival of deformation waves in the lithosphere (propagating with a velocity of about 100 km per year) at the Arctic shelf and adjacent land from the Aleutian subduction zone, the region of their generation. The trigger mechanism causing the methane release from permafrost and metastable gas hydrates is related to the destruction of micro-sized ice films covering gas hydrate particles, the elements highly important for hydrate self-preservation, as well as destruction of gas-saturated micropores in permafrost rocks due to the slight additional stresses associated with deformation waves, and thus emergence of conditions favorable for gas filtration and its subsequent emission.
format Article in Journal/Newspaper
author Leopold Lobkovsky
author_facet Leopold Lobkovsky
author_sort Leopold Lobkovsky
title Seismogenic-Triggering Mechanism of Gas Emission Activizations on the Arctic Shelf and Associated Phases of Abrupt Warming
title_short Seismogenic-Triggering Mechanism of Gas Emission Activizations on the Arctic Shelf and Associated Phases of Abrupt Warming
title_full Seismogenic-Triggering Mechanism of Gas Emission Activizations on the Arctic Shelf and Associated Phases of Abrupt Warming
title_fullStr Seismogenic-Triggering Mechanism of Gas Emission Activizations on the Arctic Shelf and Associated Phases of Abrupt Warming
title_full_unstemmed Seismogenic-Triggering Mechanism of Gas Emission Activizations on the Arctic Shelf and Associated Phases of Abrupt Warming
title_sort seismogenic-triggering mechanism of gas emission activizations on the arctic shelf and associated phases of abrupt warming
publisher MDPI AG
publishDate 2020
url https://doi.org/10.3390/geosciences10110428
https://doaj.org/article/0af00fe100484431bec44fe53c83c530
geographic Arctic
geographic_facet Arctic
genre Aleutian Island
Arctic
Ice
permafrost
genre_facet Aleutian Island
Arctic
Ice
permafrost
op_source Geosciences, Vol 10, Iss 428, p 428 (2020)
op_relation https://www.mdpi.com/2076-3263/10/11/428
https://doaj.org/toc/2076-3263
doi:10.3390/geosciences10110428
2076-3263
https://doaj.org/article/0af00fe100484431bec44fe53c83c530
op_doi https://doi.org/10.3390/geosciences10110428
container_title Geosciences
container_volume 10
container_issue 11
container_start_page 428
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