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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Istituto Nazionale di Geofisica e Vulcanologia (INGV)
1999-06-01
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Online Access: | http://www.annalsofgeophysics.eu/index.php/annals/article/view/3711 |
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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 |
_version_ |
1725763375103737856 |