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Low-latitude conjugate ULF observation by rulfmeters
https://nipr.repo.nii.ac.jp/records/1592
https://nipr.repo.nii.ac.jp/records/15927c680828-3c1f-4491-ad20-f768fb1b1e43
名前 / ファイル | ライセンス | アクション |
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KJ00000012225 (1.7 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1984-07-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Low-latitude conjugate ULF observation by rulfmeters | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Saito, Takao
× Saito, Takao× Yumoto, Kiyohumi× Seto, Masahiro× Cole, K.× Dyson, P.× Ward, J.× Gibson-Wilde, B. |
|||||
著者所属(英) | ||||||
en | ||||||
Onagawa Magnetic Observatory and Geophysical Institute, Tohoku University/Onagawa Magnetic Observatory and Geophysical Institute, Tohoku University/Tohoku Institute of Technology/School of Physical Science, La Trobe University/School of Physical Science, La Trobe University/Physics Department, James Cook University/Physics Department, James Cook University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | In order to identify the HM wave modes for low-latitude Pc 3 pulsations, it is important to observe ULF waves with some standardized magnetometers simultaneously at low-latitude conjugate stations. Hence, an intercontinental ULF observation was carried out from November 1982 to June 1983 at the three low-latitude stations; Onagawa (ONW), Japan, Townsville (TSV), Northern Australia, and Beveridge (BVR), Southern Australia. New ring-core type ULF magnetometers (rulfmeters) were set at the three sites. ONW (L=1.30) and TSV (L=1.29) are nearly conjugated magnetically, while ONW (38°.4) and BVR (-37°.8) are nearly at the same geographic latitude. Analyses were made to obtain various wave characteristics including polarization and orientation angle of Pc 3 ellipses, their diurnal behavior, etc. The results suggest a diurnal tendency that the low-latitude Pc 3 is due mainly to the compressional mode in 18-21 and 0-(8) UT, while the fundamental standing Alfven mode in 21-24 UT in these meridians. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00733561 | |||||
書誌情報 |
Memoirs of National Institute of Polar Research. Special issue 巻 31, p. 52-62, 発行日 1984-07 |