Geomagnetic polar observatories: the role of Concordia station at Dome C, Antarctica
A geomagnetic observatory is a permanent facility where magnetic declination and inclination are recorded in conjunction with the temporal evolution of the magnetic field components. Polar regions are scarcely covered by observational points then the contributions from observatories located there ar...
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Istituto Nazionale di Geofisica e Vulcanologia (INGV)
2015
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ftdoajarticles:oai:doaj.org/article:aefb91c3d49e4d648815904edcd5d9b7 2023-05-15T13:41:14+02:00 Geomagnetic polar observatories: the role of Concordia station at Dome C, Antarctica Domenico Di Mauro Lili Cafarella Stefania Lepidi Manuela Pietrolungo Laura Alfonsi Aude Chambodut 2015-03-01T00:00:00Z https://doi.org/10.4401/ag-6605 https://doaj.org/article/aefb91c3d49e4d648815904edcd5d9b7 EN eng Istituto Nazionale di Geofisica e Vulcanologia (INGV) http://www.annalsofgeophysics.eu/index.php/annals/article/view/6605 https://doaj.org/toc/1593-5213 https://doaj.org/toc/2037-416X 1593-5213 2037-416X doi:10.4401/ag-6605 https://doaj.org/article/aefb91c3d49e4d648815904edcd5d9b7 Annals of Geophysics, Vol 57, Iss 6 (2015) Geomagnetic observatory GNSS Azimuth Mark Determination Dome C Concordia Antarctica Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 article 2015 ftdoajarticles https://doi.org/10.4401/ag-6605 2022-12-30T20:57:41Z A geomagnetic observatory is a permanent facility where magnetic declination and inclination are recorded in conjunction with the temporal evolution of the magnetic field components. Polar regions are scarcely covered by observational points then the contributions from observatories located there are particularly relevant. The geomagnetic observatory at Concordia station, Dome C - Antarctica is located in the inner part of the continent, its position is favorable for two key reasons, i) data are unaltered by the "coastal effect” and ii) crustal effect is negligible due to the thickness, almost 3 km, of ice coverage. Nevertheless, these latter conditions imply an unconsidered aspect which characterizes the entire station and every structure laying on the ice surface: the dome on which Concordia station resides is sliding horizontally and moving vertically with a velocity of few millimeter to centimeters per year as indicated by independent geodetic observations. This slow and continuous movement has a puzzling effect on the trend of horizontal components of the magnetic field, sampled in a time window of a decade since the establishing of the observatory in 2005. During the International Polar Year (2007-2009) the observatory was upgraded with new equipment fulfilling the requirements of the Intermagnet consortium, and becoming an observatory member in 2011. In this paper are illustrated the strategy adopted to track any possible displacement of the observatory reference points (i.e. the azimuth mark, the pillar position) and all the ordinary and extraordinary actions required for collecting high quality data. Article in Journal/Newspaper Antarc* Antarctica International Polar Year Directory of Open Access Journals: DOAJ Articles Concordia Station ENVELOPE(123.333,123.333,-75.100,-75.100) Pillar ENVELOPE(166.217,166.217,-77.583,-77.583) The Pillar ENVELOPE(-126.853,-126.853,57.300,57.300) Annals of Geophysics 57 6 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Geomagnetic observatory GNSS Azimuth Mark Determination Dome C Concordia Antarctica Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 |
spellingShingle |
Geomagnetic observatory GNSS Azimuth Mark Determination Dome C Concordia Antarctica Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 Domenico Di Mauro Lili Cafarella Stefania Lepidi Manuela Pietrolungo Laura Alfonsi Aude Chambodut Geomagnetic polar observatories: the role of Concordia station at Dome C, Antarctica |
topic_facet |
Geomagnetic observatory GNSS Azimuth Mark Determination Dome C Concordia Antarctica Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 |
description |
A geomagnetic observatory is a permanent facility where magnetic declination and inclination are recorded in conjunction with the temporal evolution of the magnetic field components. Polar regions are scarcely covered by observational points then the contributions from observatories located there are particularly relevant. The geomagnetic observatory at Concordia station, Dome C - Antarctica is located in the inner part of the continent, its position is favorable for two key reasons, i) data are unaltered by the "coastal effect” and ii) crustal effect is negligible due to the thickness, almost 3 km, of ice coverage. Nevertheless, these latter conditions imply an unconsidered aspect which characterizes the entire station and every structure laying on the ice surface: the dome on which Concordia station resides is sliding horizontally and moving vertically with a velocity of few millimeter to centimeters per year as indicated by independent geodetic observations. This slow and continuous movement has a puzzling effect on the trend of horizontal components of the magnetic field, sampled in a time window of a decade since the establishing of the observatory in 2005. During the International Polar Year (2007-2009) the observatory was upgraded with new equipment fulfilling the requirements of the Intermagnet consortium, and becoming an observatory member in 2011. In this paper are illustrated the strategy adopted to track any possible displacement of the observatory reference points (i.e. the azimuth mark, the pillar position) and all the ordinary and extraordinary actions required for collecting high quality data. |
format |
Article in Journal/Newspaper |
author |
Domenico Di Mauro Lili Cafarella Stefania Lepidi Manuela Pietrolungo Laura Alfonsi Aude Chambodut |
author_facet |
Domenico Di Mauro Lili Cafarella Stefania Lepidi Manuela Pietrolungo Laura Alfonsi Aude Chambodut |
author_sort |
Domenico Di Mauro |
title |
Geomagnetic polar observatories: the role of Concordia station at Dome C, Antarctica |
title_short |
Geomagnetic polar observatories: the role of Concordia station at Dome C, Antarctica |
title_full |
Geomagnetic polar observatories: the role of Concordia station at Dome C, Antarctica |
title_fullStr |
Geomagnetic polar observatories: the role of Concordia station at Dome C, Antarctica |
title_full_unstemmed |
Geomagnetic polar observatories: the role of Concordia station at Dome C, Antarctica |
title_sort |
geomagnetic polar observatories: the role of concordia station at dome c, antarctica |
publisher |
Istituto Nazionale di Geofisica e Vulcanologia (INGV) |
publishDate |
2015 |
url |
https://doi.org/10.4401/ag-6605 https://doaj.org/article/aefb91c3d49e4d648815904edcd5d9b7 |
long_lat |
ENVELOPE(123.333,123.333,-75.100,-75.100) ENVELOPE(166.217,166.217,-77.583,-77.583) ENVELOPE(-126.853,-126.853,57.300,57.300) |
geographic |
Concordia Station Pillar The Pillar |
geographic_facet |
Concordia Station Pillar The Pillar |
genre |
Antarc* Antarctica International Polar Year |
genre_facet |
Antarc* Antarctica International Polar Year |
op_source |
Annals of Geophysics, Vol 57, Iss 6 (2015) |
op_relation |
http://www.annalsofgeophysics.eu/index.php/annals/article/view/6605 https://doaj.org/toc/1593-5213 https://doaj.org/toc/2037-416X 1593-5213 2037-416X doi:10.4401/ag-6605 https://doaj.org/article/aefb91c3d49e4d648815904edcd5d9b7 |
op_doi |
https://doi.org/10.4401/ag-6605 |
container_title |
Annals of Geophysics |
container_volume |
57 |
container_issue |
6 |
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1766148107007950848 |