On feasibility to detect volcanoes hidden under the ice of Antarctica via their "gravitational signal"
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985815%3A_____%2F16%3A00470516" target="_blank" >RIV/67985815:_____/16:00470516 - isvavai.cz</a>
Alternative codes found
RIV/61989100:27350/16:86098993 RIV/00025615:_____/16:N0000020 RIV/68407700:21110/16:00346679
Result on the web
<a href="http://dx.doi.org/10.4401/ag-7102" target="_blank" >http://dx.doi.org/10.4401/ag-7102</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.4401/ag-7102" target="_blank" >10.4401/ag-7102</a>
Alternative languages
Result language
angličtina
Original language name
On feasibility to detect volcanoes hidden under the ice of Antarctica via their "gravitational signal"
Original language 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.
Czech name
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DC - Seismology, volcanology and Earth structure
OECD FORD branch
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Result continuities
Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2016
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Annals of Geophysics
ISSN
1593-5213
e-ISSN
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Volume of the periodical
59
Issue of the periodical within the volume
5
Country of publishing house
IT - ITALY
Number of pages
22
Pages from-to
"S0539/1"-"S0539/22"
UT code for WoS article
000389932200009
EID of the result in the Scopus database
2-s2.0-84997132430