Comparison of K-index Calculations between Several Geomagnetic Stations during IQDs and IDDs

BOH magnetometer was installed at Mt. Bohyun in 2007 and has provided continuous dataset for 3-axis geomagnetic field over the South Korea. We have calculated real-time K-index based on BOH magnetic field data using well-known FMI method. Local K-index is calculated eight times a day, per every th...

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Main Authors: Junga Hwang, Hang-Pyo Kim, Young-Deuk Park
Format: Article
Language:English
Published: Korean Space Science Society (KSSS) 2013-09-01
Series:Journal of Astronomy and Space Sciences
Subjects:
Online Access:http://ocean.kisti.re.kr/downfile/volume/kosss/OJOOBS/2013/v30n3/OJOOBS_2013_v30n3_169.pdf
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spelling doaj-82322f9c1e0145269b0219be07e244732020-11-25T00:32:56ZengKorean Space Science Society (KSSS)Journal of Astronomy and Space Sciences2093-55872093-14092013-09-0130316917410.5140/JASS.2013.30.3.169Comparison of K-index Calculations between Several Geomagnetic Stations during IQDs and IDDsJunga Hwang0Hang-Pyo Kim1Young-Deuk Park2Korea Astronomy and Space Science Institute, Daejeon 305-348, KoreaKorea Astronomy and Space Science Institute, Daejeon 305-348, KoreaKorea Astronomy and Space Science Institute, Daejeon 305-348, KoreaBOH magnetometer was installed at Mt. Bohyun in 2007 and has provided continuous dataset for 3-axis geomagnetic field over the South Korea. We have calculated real-time K-index based on BOH magnetic field data using well-known FMI method. Local K-index is calculated eight times a day, per every three hours. To calculate K-index, it is critical to get the Quiet Day Curve (QDC). For QDC calculation, we take the previous one month’s average of H-component. In this paper, we compared four geomagnetic stations’ magnetic field data over South Korea and Japan and K-indices of each stations; Bohyun, Gangneung, Jeju, and Kakioka for two years data, 2011-2012. To investigate the difference depending on the latitude, longitude and local time in more detail, we compare K-index on International Quiet Days (IQDs) and International Disturbed Days (IDDs). As a result, we report the correlation between local K-indices are higher than those between Kp and local K-indices, and the correlation is much better after sunset than after sunrise. As the geomagnetic activity becomes stronger, the correlation between the local K-indices and global Kp-index become higher.http://ocean.kisti.re.kr/downfile/volume/kosss/OJOOBS/2013/v30n3/OJOOBS_2013_v30n3_169.pdfK-indexBOH magnetometerIQDs and IDDs
collection DOAJ
language English
format Article
sources DOAJ
author Junga Hwang
Hang-Pyo Kim
Young-Deuk Park
spellingShingle Junga Hwang
Hang-Pyo Kim
Young-Deuk Park
Comparison of K-index Calculations between Several Geomagnetic Stations during IQDs and IDDs
Journal of Astronomy and Space Sciences
K-index
BOH magnetometer
IQDs and IDDs
author_facet Junga Hwang
Hang-Pyo Kim
Young-Deuk Park
author_sort Junga Hwang
title Comparison of K-index Calculations between Several Geomagnetic Stations during IQDs and IDDs
title_short Comparison of K-index Calculations between Several Geomagnetic Stations during IQDs and IDDs
title_full Comparison of K-index Calculations between Several Geomagnetic Stations during IQDs and IDDs
title_fullStr Comparison of K-index Calculations between Several Geomagnetic Stations during IQDs and IDDs
title_full_unstemmed Comparison of K-index Calculations between Several Geomagnetic Stations during IQDs and IDDs
title_sort comparison of k-index calculations between several geomagnetic stations during iqds and idds
publisher Korean Space Science Society (KSSS)
series Journal of Astronomy and Space Sciences
issn 2093-5587
2093-1409
publishDate 2013-09-01
description BOH magnetometer was installed at Mt. Bohyun in 2007 and has provided continuous dataset for 3-axis geomagnetic field over the South Korea. We have calculated real-time K-index based on BOH magnetic field data using well-known FMI method. Local K-index is calculated eight times a day, per every three hours. To calculate K-index, it is critical to get the Quiet Day Curve (QDC). For QDC calculation, we take the previous one month’s average of H-component. In this paper, we compared four geomagnetic stations’ magnetic field data over South Korea and Japan and K-indices of each stations; Bohyun, Gangneung, Jeju, and Kakioka for two years data, 2011-2012. To investigate the difference depending on the latitude, longitude and local time in more detail, we compare K-index on International Quiet Days (IQDs) and International Disturbed Days (IDDs). As a result, we report the correlation between local K-indices are higher than those between Kp and local K-indices, and the correlation is much better after sunset than after sunrise. As the geomagnetic activity becomes stronger, the correlation between the local K-indices and global Kp-index become higher.
topic K-index
BOH magnetometer
IQDs and IDDs
url http://ocean.kisti.re.kr/downfile/volume/kosss/OJOOBS/2013/v30n3/OJOOBS_2013_v30n3_169.pdf
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