Geomagnetic observations on Tristan da Cunha, South Atlantic Ocean

Few geomagnetic ground observations exist of the Earth’s strongest core field anomaly, the South Atlantic Anomaly (SAA). The geomagnetic repeat station on the island Tristan da Cunha, located half-way between South Africa and South America at 37° 05’ S, 12° 18’ W, is therefore of crucial importance....

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Published in:Annals of Geophysics
Main Authors: Susan Macmillan, Alan M. Berarducci, Lars William Pedersen, Cathrine Fox Maule, Nils Olsen, Jürgen Matzka
Format: Article in Journal/Newspaper
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2009
Subjects:
Online Access:https://doi.org/10.4401/ag-4633
https://doaj.org/article/d76c20c9e2084376851eb189a5e747d0
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spelling ftdoajarticles:oai:doaj.org/article:d76c20c9e2084376851eb189a5e747d0 2023-05-15T18:21:05+02:00 Geomagnetic observations on Tristan da Cunha, South Atlantic Ocean Susan Macmillan Alan M. Berarducci Lars William Pedersen Cathrine Fox Maule Nils Olsen Jürgen Matzka 2009-06-01T00:00:00Z https://doi.org/10.4401/ag-4633 https://doaj.org/article/d76c20c9e2084376851eb189a5e747d0 EN eng Istituto Nazionale di Geofisica e Vulcanologia (INGV) http://www.annalsofgeophysics.eu/index.php/annals/article/view/4633 https://doaj.org/toc/1593-5213 https://doaj.org/toc/2037-416X doi:10.4401/ag-4633 1593-5213 2037-416X https://doaj.org/article/d76c20c9e2084376851eb189a5e747d0 Annals of Geophysics, Vol 52, Iss 1, Pp 97-105 (2009) South Atlantic Anomaly – geomagnetic observatory – geomagnetic repeat station – Tristan da Cunha Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 article 2009 ftdoajarticles https://doi.org/10.4401/ag-4633 2022-12-31T07:04:45Z Few geomagnetic ground observations exist of the Earth’s strongest core field anomaly, the South Atlantic Anomaly (SAA). The geomagnetic repeat station on the island Tristan da Cunha, located half-way between South Africa and South America at 37° 05’ S, 12° 18’ W, is therefore of crucial importance. We have conducted several sets of repeat station measurements during magnetically quiet conditions (Kp 2o or less) in 2004. The procedures are described and the results are compared to those from earlier campaigns and to the predictions of various global field models. Features of the local crustal bias field and the solar quiet daily variation are discussed. We also evaluate the benefit of continuous magnetic field recordings from Tristan da Cunha, and argue that such a data set is a very valuable addition to geomagnetic satellite data. Recently, funds were set up to establish and operate a magnetometer station on Tristan da Cunha during the Swarm magnetic satellite mission (2011-2014). Article in Journal/Newspaper South Atlantic Ocean Directory of Open Access Journals: DOAJ Articles Tristan ENVELOPE(140.900,140.900,-66.735,-66.735) Annals of Geophysics 52 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic South Atlantic Anomaly – geomagnetic observatory – geomagnetic repeat station – Tristan da Cunha
Meteorology. Climatology
QC851-999
Geophysics. Cosmic physics
QC801-809
spellingShingle South Atlantic Anomaly – geomagnetic observatory – geomagnetic repeat station – Tristan da Cunha
Meteorology. Climatology
QC851-999
Geophysics. Cosmic physics
QC801-809
Susan Macmillan
Alan M. Berarducci
Lars William Pedersen
Cathrine Fox Maule
Nils Olsen
Jürgen Matzka
Geomagnetic observations on Tristan da Cunha, South Atlantic Ocean
topic_facet South Atlantic Anomaly – geomagnetic observatory – geomagnetic repeat station – Tristan da Cunha
Meteorology. Climatology
QC851-999
Geophysics. Cosmic physics
QC801-809
description Few geomagnetic ground observations exist of the Earth’s strongest core field anomaly, the South Atlantic Anomaly (SAA). The geomagnetic repeat station on the island Tristan da Cunha, located half-way between South Africa and South America at 37° 05’ S, 12° 18’ W, is therefore of crucial importance. We have conducted several sets of repeat station measurements during magnetically quiet conditions (Kp 2o or less) in 2004. The procedures are described and the results are compared to those from earlier campaigns and to the predictions of various global field models. Features of the local crustal bias field and the solar quiet daily variation are discussed. We also evaluate the benefit of continuous magnetic field recordings from Tristan da Cunha, and argue that such a data set is a very valuable addition to geomagnetic satellite data. Recently, funds were set up to establish and operate a magnetometer station on Tristan da Cunha during the Swarm magnetic satellite mission (2011-2014).
format Article in Journal/Newspaper
author Susan Macmillan
Alan M. Berarducci
Lars William Pedersen
Cathrine Fox Maule
Nils Olsen
Jürgen Matzka
author_facet Susan Macmillan
Alan M. Berarducci
Lars William Pedersen
Cathrine Fox Maule
Nils Olsen
Jürgen Matzka
author_sort Susan Macmillan
title Geomagnetic observations on Tristan da Cunha, South Atlantic Ocean
title_short Geomagnetic observations on Tristan da Cunha, South Atlantic Ocean
title_full Geomagnetic observations on Tristan da Cunha, South Atlantic Ocean
title_fullStr Geomagnetic observations on Tristan da Cunha, South Atlantic Ocean
title_full_unstemmed Geomagnetic observations on Tristan da Cunha, South Atlantic Ocean
title_sort geomagnetic observations on tristan da cunha, south atlantic ocean
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
publishDate 2009
url https://doi.org/10.4401/ag-4633
https://doaj.org/article/d76c20c9e2084376851eb189a5e747d0
long_lat ENVELOPE(140.900,140.900,-66.735,-66.735)
geographic Tristan
geographic_facet Tristan
genre South Atlantic Ocean
genre_facet South Atlantic Ocean
op_source Annals of Geophysics, Vol 52, Iss 1, Pp 97-105 (2009)
op_relation http://www.annalsofgeophysics.eu/index.php/annals/article/view/4633
https://doaj.org/toc/1593-5213
https://doaj.org/toc/2037-416X
doi:10.4401/ag-4633
1593-5213
2037-416X
https://doaj.org/article/d76c20c9e2084376851eb189a5e747d0
op_doi https://doi.org/10.4401/ag-4633
container_title Annals of Geophysics
container_volume 52
container_issue 1
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