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| ファイル | 記述 | サイズ | フォーマット | |
|---|---|---|---|---|
| sgk00800_009.pdf | 323.28 kB | Adobe PDF | 見る/開く |
完全メタデータレコード
| DCフィールド | 値 | 言語 |
|---|---|---|
| dc.contributor.author | MURATA, Hiroo | en |
| dc.date.accessioned | 2013-09-02T04:23:36Z | - |
| dc.date.available | 2013-09-02T04:23:36Z | - |
| dc.date.issued | 1968-12 | - |
| dc.identifier.issn | 0454-7837 | - |
| dc.identifier.uri | http://hdl.handle.net/2433/178562 | - |
| dc.description.abstract | The purpose of the present paper is to analyse the seasonal variation of the geomagnetic D-component of Sq at five selected magnetic observatories near the dipequator, by using data on magnetically quiet days during the IGY. The result shows a persistent winter-summer symmetry in such a way that its variation has a maximum value at about 0.7 L.T. (= 15 r) and 18 L.T. (= 5 r) and a minimum value at about 12 L.T. C= -15 r) for summer, and the sign of its variation is inversed for winter. It will be discussed as to why these variations of the D-component occurred. | en |
| dc.format.mimetype | application/pdf | - |
| dc.language.iso | eng | - |
| dc.publisher | Geophysical Institute, Kyoto University | en |
| dc.subject.ndc | 450 | - |
| dc.title | SEASONAL VARIATION IN THE D-COMPONENT OF Sq NEAR THE DIP-EQUATOR | en |
| dc.type | departmental bulletin paper | - |
| dc.type.niitype | Departmental Bulletin Paper | - |
| dc.identifier.ncid | AA00423961 | - |
| dc.identifier.jtitle | Special Contributions of the Geophysical Institute, Kyoto University | en |
| dc.identifier.volume | 8 | - |
| dc.identifier.spage | 9 | - |
| dc.identifier.epage | 14 | - |
| dc.textversion | publisher | - |
| dc.sortkey | 03 | - |
| dcterms.accessRights | open access | - |
| dc.identifier.pissn | 0454-7837 | - |
| 出現コレクション: | No.8 | |
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