The Distribution of Geomagnetic Field Components on the Southern Part of the Korean Peninsula for Epoch 2010.0

NGII(National Geography Information Institute) of Korea consigned KIGAM(Korea Institute of Geoscience & Mineral Resources) to do absolute geomagnetic measurements on 32 geomagnetic repeat stations evenly distributed on the southern part of Korean Peninsula in the year 2010 and to produce geomagn...

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Main Authors: Mutaek Lim, Jiyoung Moon, Yeongsue Park, Younghong Shin, Hyoungrae Rim
Format: Article
Language:English
Published: Ubiquity Press 2011-05-01
Series:Data Science Journal
Subjects:
Online Access:http://datascience.codata.org/articles/104
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spelling doaj-002b52c3e77743d9abb1712b034506232020-11-24T22:18:44ZengUbiquity PressData Science Journal1683-14702011-05-011010.2481/dsj.IAGA-12104The Distribution of Geomagnetic Field Components on the Southern Part of the Korean Peninsula for Epoch 2010.0Mutaek Lim0Jiyoung Moon1Yeongsue Park2Younghong Shin3Hyoungrae Rim4Korea Institute of Geoscience & Mineral Resources, 92 Gwahang-no, Yuseong-gu, Daejeon, 305-350, KoreaNational Geography Information Institute, 587 Worldcup-gil, Yeongtong-gu, Suwon, Gyeonggi-do, 443-772, KoreaKorea Institute of Geoscience & Mineral Resources, 92 Gwahang-no, Yuseong-gu, Daejeon, 305-350, KoreaKorea Institute of Geoscience & Mineral Resources, 92 Gwahang-no, Yuseong-gu, Daejeon, 305-350, KoreaKorea Institute of Geoscience & Mineral Resources, 92 Gwahang-no, Yuseong-gu, Daejeon, 305-350, KoreaNGII(National Geography Information Institute) of Korea consigned KIGAM(Korea Institute of Geoscience & Mineral Resources) to do absolute geomagnetic measurements on 32 geomagnetic repeat stations evenly distributed on the southern part of Korean Peninsula in the year 2010 and to produce geomagnetic field components' distribution maps for the year 2010.0. The result of the processing of the measured data, i. e., the geomagnetic field components' distribution, shows a near similarity with that calculated from IGRF-11 although the latter was processed without any real geomagnetic data measured on the Korean Peninsula as an input. This implies that we installed the repeat stations on sites with good geomagnetic conditions and that our result in accordance with the IGRF represents well the regional distribution trend, i. e., it is dominated by relatively long wavelength components.http://datascience.codata.org/articles/104GeomagnetismDeclinationInclinationTotal magnetic intensityDistributionKorean Peninsula
collection DOAJ
language English
format Article
sources DOAJ
author Mutaek Lim
Jiyoung Moon
Yeongsue Park
Younghong Shin
Hyoungrae Rim
spellingShingle Mutaek Lim
Jiyoung Moon
Yeongsue Park
Younghong Shin
Hyoungrae Rim
The Distribution of Geomagnetic Field Components on the Southern Part of the Korean Peninsula for Epoch 2010.0
Data Science Journal
Geomagnetism
Declination
Inclination
Total magnetic intensity
Distribution
Korean Peninsula
author_facet Mutaek Lim
Jiyoung Moon
Yeongsue Park
Younghong Shin
Hyoungrae Rim
author_sort Mutaek Lim
title The Distribution of Geomagnetic Field Components on the Southern Part of the Korean Peninsula for Epoch 2010.0
title_short The Distribution of Geomagnetic Field Components on the Southern Part of the Korean Peninsula for Epoch 2010.0
title_full The Distribution of Geomagnetic Field Components on the Southern Part of the Korean Peninsula for Epoch 2010.0
title_fullStr The Distribution of Geomagnetic Field Components on the Southern Part of the Korean Peninsula for Epoch 2010.0
title_full_unstemmed The Distribution of Geomagnetic Field Components on the Southern Part of the Korean Peninsula for Epoch 2010.0
title_sort distribution of geomagnetic field components on the southern part of the korean peninsula for epoch 2010.0
publisher Ubiquity Press
series Data Science Journal
issn 1683-1470
publishDate 2011-05-01
description NGII(National Geography Information Institute) of Korea consigned KIGAM(Korea Institute of Geoscience & Mineral Resources) to do absolute geomagnetic measurements on 32 geomagnetic repeat stations evenly distributed on the southern part of Korean Peninsula in the year 2010 and to produce geomagnetic field components' distribution maps for the year 2010.0. The result of the processing of the measured data, i. e., the geomagnetic field components' distribution, shows a near similarity with that calculated from IGRF-11 although the latter was processed without any real geomagnetic data measured on the Korean Peninsula as an input. This implies that we installed the repeat stations on sites with good geomagnetic conditions and that our result in accordance with the IGRF represents well the regional distribution trend, i. e., it is dominated by relatively long wavelength components.
topic Geomagnetism
Declination
Inclination
Total magnetic intensity
Distribution
Korean Peninsula
url http://datascience.codata.org/articles/104
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