Measurements of vector magnetic anomalies on board the icebreaker Shirase and the magnetization of the ship

Vector measurements of the geomagnetic field have been made in the South Indian Ocean since 1988 when a Shipboard Three Component Magnetometer (STCM) was installed on board the icebreaker Shirase by the 30th Japanese Antarctic Research Expedition (JARE-30). Twelve constants related to the ship'...

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Published in:Annals of Geophysics
Main Authors: K. Kaminuma, Y. Nogi
Format: Article in Journal/Newspaper
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1999
Subjects:
Online Access:https://doi.org/10.4401/ag-3711
https://doaj.org/article/29d98728c5df4b2f97e3db530d793daf
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spelling ftdoajarticles:oai:doaj.org/article:29d98728c5df4b2f97e3db530d793daf 2023-05-15T13:56:03+02:00 Measurements of vector magnetic anomalies on board the icebreaker Shirase and the magnetization of the ship K. Kaminuma Y. Nogi 1999-06-01T00:00:00Z https://doi.org/10.4401/ag-3711 https://doaj.org/article/29d98728c5df4b2f97e3db530d793daf EN eng Istituto Nazionale di Geofisica e Vulcanologia (INGV) http://www.annalsofgeophysics.eu/index.php/annals/article/view/3711 https://doaj.org/toc/1593-5213 https://doaj.org/toc/2037-416X doi:10.4401/ag-3711 1593-5213 2037-416X https://doaj.org/article/29d98728c5df4b2f97e3db530d793daf Annals of Geophysics, Vol 42, Iss 2 (1999) shipboard three component magnetometer vector measurements of the geomagnetic field ship's permanent magnetization ship's induced magnetic field Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 article 1999 ftdoajarticles https://doi.org/10.4401/ag-3711 2022-12-31T06:43:37Z Vector measurements of the geomagnetic field have been made in the South Indian Ocean since 1988 when a Shipboard Three Component Magnetometer (STCM) was installed on board the icebreaker Shirase by the 30th Japanese Antarctic Research Expedition (JARE-30). Twelve constants related to the ship's induced and permanent magnetic field were determined by the data obtained from the JARE-30 to the JARE-35. The constants related to the ship's magnetic susceptibility distribution are almost stable throughout the cruise and mostly depend on the ship's shape. On the other hand, the constants related to the ship's permanent magnetization are variable. However, absolute values of total intensity geomagnetic field calculated from vector geomagnetic field is possible to use, if the constraints from total intensity geomagnetic field measured by the proton magnetometer and/or satellite derived magnetic anomalies are applied. Article in Journal/Newspaper Antarc* Antarctic Icebreaker Directory of Open Access Journals: DOAJ Articles Antarctic Indian Annals of Geophysics 42 2
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic shipboard three component magnetometer
vector measurements of the geomagnetic field
ship's permanent magnetization
ship's induced magnetic field
Meteorology. Climatology
QC851-999
Geophysics. Cosmic physics
QC801-809
spellingShingle shipboard three component magnetometer
vector measurements of the geomagnetic field
ship's permanent magnetization
ship's induced magnetic field
Meteorology. Climatology
QC851-999
Geophysics. Cosmic physics
QC801-809
K. Kaminuma
Y. Nogi
Measurements of vector magnetic anomalies on board the icebreaker Shirase and the magnetization of the ship
topic_facet shipboard three component magnetometer
vector measurements of the geomagnetic field
ship's permanent magnetization
ship's induced magnetic field
Meteorology. Climatology
QC851-999
Geophysics. Cosmic physics
QC801-809
description Vector measurements of the geomagnetic field have been made in the South Indian Ocean since 1988 when a Shipboard Three Component Magnetometer (STCM) was installed on board the icebreaker Shirase by the 30th Japanese Antarctic Research Expedition (JARE-30). Twelve constants related to the ship's induced and permanent magnetic field were determined by the data obtained from the JARE-30 to the JARE-35. The constants related to the ship's magnetic susceptibility distribution are almost stable throughout the cruise and mostly depend on the ship's shape. On the other hand, the constants related to the ship's permanent magnetization are variable. However, absolute values of total intensity geomagnetic field calculated from vector geomagnetic field is possible to use, if the constraints from total intensity geomagnetic field measured by the proton magnetometer and/or satellite derived magnetic anomalies are applied.
format Article in Journal/Newspaper
author K. Kaminuma
Y. Nogi
author_facet K. Kaminuma
Y. Nogi
author_sort K. Kaminuma
title Measurements of vector magnetic anomalies on board the icebreaker Shirase and the magnetization of the ship
title_short Measurements of vector magnetic anomalies on board the icebreaker Shirase and the magnetization of the ship
title_full Measurements of vector magnetic anomalies on board the icebreaker Shirase and the magnetization of the ship
title_fullStr Measurements of vector magnetic anomalies on board the icebreaker Shirase and the magnetization of the ship
title_full_unstemmed Measurements of vector magnetic anomalies on board the icebreaker Shirase and the magnetization of the ship
title_sort measurements of vector magnetic anomalies on board the icebreaker shirase and the magnetization of the ship
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
publishDate 1999
url https://doi.org/10.4401/ag-3711
https://doaj.org/article/29d98728c5df4b2f97e3db530d793daf
geographic Antarctic
Indian
geographic_facet Antarctic
Indian
genre Antarc*
Antarctic
Icebreaker
genre_facet Antarc*
Antarctic
Icebreaker
op_source Annals of Geophysics, Vol 42, Iss 2 (1999)
op_relation http://www.annalsofgeophysics.eu/index.php/annals/article/view/3711
https://doaj.org/toc/1593-5213
https://doaj.org/toc/2037-416X
doi:10.4401/ag-3711
1593-5213
2037-416X
https://doaj.org/article/29d98728c5df4b2f97e3db530d793daf
op_doi https://doi.org/10.4401/ag-3711
container_title Annals of Geophysics
container_volume 42
container_issue 2
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