On feasibility to detect volcanoes hidden under the ice of Antarctica via their “gravitational signal”

Many undiscovered volcanoes may be hidden under the thick layers of the ice of Antarctica. Hypothetic volcanoes were sought by means of the best present-day gravitational data (gravity field model EIGEN 6C4) and bedrock topography data (Bedmap2). A new previously unused method was tested. The analog...

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Published in:Annals of Geophysics
Main Authors: Jaroslav Klokočník, Jan Kostelecký, Ivan Pešek, Aleš Bezděk
Format: Article in Journal/Newspaper
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2016
Subjects:
Online Access:https://doi.org/10.4401/ag-7102
https://doaj.org/article/87911ae1016144328603d96a1a5ecdde
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spelling ftdoajarticles:oai:doaj.org/article:87911ae1016144328603d96a1a5ecdde 2023-05-15T13:34:06+02:00 On feasibility to detect volcanoes hidden under the ice of Antarctica via their “gravitational signal” Jaroslav Klokočník Jan Kostelecký Ivan Pešek Aleš Bezděk 2016-11-01T00:00:00Z https://doi.org/10.4401/ag-7102 https://doaj.org/article/87911ae1016144328603d96a1a5ecdde EN eng Istituto Nazionale di Geofisica e Vulcanologia (INGV) http://www.annalsofgeophysics.eu/index.php/annals/article/view/7102 https://doaj.org/toc/1593-5213 https://doaj.org/toc/2037-416X 1593-5213 2037-416X doi:10.4401/ag-7102 https://doaj.org/article/87911ae1016144328603d96a1a5ecdde Annals of Geophysics, Vol 59, Iss 5 (2016) Gravity field model EIGEN 6C4 Functions of disturbing potential Volcanoes Antarctica Bedmap2 RET 14 Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 article 2016 ftdoajarticles https://doi.org/10.4401/ag-7102 2022-12-31T00:01:03Z Many undiscovered volcanoes may be hidden under the thick layers of the ice of Antarctica. Hypothetic volcanoes were sought by means of the best present-day gravitational data (gravity field model EIGEN 6C4) and bedrock topography data (Bedmap2). A new previously unused method was tested. The analogy with the “gravitational signal” typical for volcanoes and other structures in other parts of the Earth is used. Various functions (not only ordinary gravity anomalies) of the disturbing geopotential were employed: Marussi tensor of the second derivatives, geopotential invariants, the strike angle and the virtual deformations. We attempted to discover if the best present-day gravitational and topographic data are of sufficient precision and resolution and how fast is the attenuation of the “gravitational signal” of a volcano with increasing depth under the ice. It is shown that there is no principal obstacle to detect volcanoes by our method. However, it appeared very quickly that our present-day attempts to discover such volcanoes could hardly be successful, mainly due to a low resolution of the existing gravity data and also due to a low resolution of the best bedrock topography of Antarctica currently available. Nevertheless, some examples of hypothetical volcanoes under the ice are given, but they are uncertain. However, the method, the main goal of this feasibility study, is ready and working. Article in Journal/Newspaper Antarc* Antarctica Directory of Open Access Journals: DOAJ Articles Annals of Geophysics 59 5
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Gravity field model EIGEN 6C4
Functions of disturbing potential
Volcanoes
Antarctica
Bedmap2
RET 14
Meteorology. Climatology
QC851-999
Geophysics. Cosmic physics
QC801-809
spellingShingle Gravity field model EIGEN 6C4
Functions of disturbing potential
Volcanoes
Antarctica
Bedmap2
RET 14
Meteorology. Climatology
QC851-999
Geophysics. Cosmic physics
QC801-809
Jaroslav Klokočník
Jan Kostelecký
Ivan Pešek
Aleš Bezděk
On feasibility to detect volcanoes hidden under the ice of Antarctica via their “gravitational signal”
topic_facet Gravity field model EIGEN 6C4
Functions of disturbing potential
Volcanoes
Antarctica
Bedmap2
RET 14
Meteorology. Climatology
QC851-999
Geophysics. Cosmic physics
QC801-809
description Many undiscovered volcanoes may be hidden under the thick layers of the ice of Antarctica. Hypothetic volcanoes were sought by means of the best present-day gravitational data (gravity field model EIGEN 6C4) and bedrock topography data (Bedmap2). A new previously unused method was tested. The analogy with the “gravitational signal” typical for volcanoes and other structures in other parts of the Earth is used. Various functions (not only ordinary gravity anomalies) of the disturbing geopotential were employed: Marussi tensor of the second derivatives, geopotential invariants, the strike angle and the virtual deformations. We attempted to discover if the best present-day gravitational and topographic data are of sufficient precision and resolution and how fast is the attenuation of the “gravitational signal” of a volcano with increasing depth under the ice. It is shown that there is no principal obstacle to detect volcanoes by our method. However, it appeared very quickly that our present-day attempts to discover such volcanoes could hardly be successful, mainly due to a low resolution of the existing gravity data and also due to a low resolution of the best bedrock topography of Antarctica currently available. Nevertheless, some examples of hypothetical volcanoes under the ice are given, but they are uncertain. However, the method, the main goal of this feasibility study, is ready and working.
format Article in Journal/Newspaper
author Jaroslav Klokočník
Jan Kostelecký
Ivan Pešek
Aleš Bezděk
author_facet Jaroslav Klokočník
Jan Kostelecký
Ivan Pešek
Aleš Bezděk
author_sort Jaroslav Klokočník
title On feasibility to detect volcanoes hidden under the ice of Antarctica via their “gravitational signal”
title_short On feasibility to detect volcanoes hidden under the ice of Antarctica via their “gravitational signal”
title_full On feasibility to detect volcanoes hidden under the ice of Antarctica via their “gravitational signal”
title_fullStr On feasibility to detect volcanoes hidden under the ice of Antarctica via their “gravitational signal”
title_full_unstemmed On feasibility to detect volcanoes hidden under the ice of Antarctica via their “gravitational signal”
title_sort on feasibility to detect volcanoes hidden under the ice of antarctica via their “gravitational signal”
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
publishDate 2016
url https://doi.org/10.4401/ag-7102
https://doaj.org/article/87911ae1016144328603d96a1a5ecdde
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Annals of Geophysics, Vol 59, Iss 5 (2016)
op_relation http://www.annalsofgeophysics.eu/index.php/annals/article/view/7102
https://doaj.org/toc/1593-5213
https://doaj.org/toc/2037-416X
1593-5213
2037-416X
doi:10.4401/ag-7102
https://doaj.org/article/87911ae1016144328603d96a1a5ecdde
op_doi https://doi.org/10.4401/ag-7102
container_title Annals of Geophysics
container_volume 59
container_issue 5
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