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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Main Authors: K. Kaminuma, Y. Nogi
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1999-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3711
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spelling doaj-29d98728c5df4b2f97e3db530d793daf2020-11-24T22:23:54ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X1999-06-0142210.4401/ag-3711Measurements of vector magnetic anomalies on board the icebreaker Shirase and the magnetization of the shipK. KaminumaY. NogiVector 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.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3711shipboard three component magnetometervector measurements of the geomagnetic fieldship's permanent magnetizationship's induced magnetic field
collection DOAJ
language English
format Article
sources DOAJ
author K. Kaminuma
Y. Nogi
spellingShingle K. Kaminuma
Y. Nogi
Measurements of vector magnetic anomalies on board the icebreaker Shirase and the magnetization of the ship
Annals of Geophysics
shipboard three component magnetometer
vector measurements of the geomagnetic field
ship's permanent magnetization
ship's induced magnetic field
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)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 1999-06-01
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.
topic shipboard three component magnetometer
vector measurements of the geomagnetic field
ship's permanent magnetization
ship's induced magnetic field
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3711
work_keys_str_mv AT kkaminuma measurementsofvectormagneticanomaliesonboardtheicebreakershiraseandthemagnetizationoftheship
AT ynogi measurementsofvectormagneticanomaliesonboardtheicebreakershiraseandthemagnetizationoftheship
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