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このアイテムのファイル:
| ファイル | 記述 | サイズ | フォーマット | |
|---|---|---|---|---|
| sgk00700_045.pdf | 644.16 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 | MAMAMOTO, Ryozaburo | en |
| dc.date.accessioned | 2013-09-02T04:22:41Z | - |
| dc.date.available | 2013-09-02T04:22:41Z | - |
| dc.date.issued | 1967-12 | - |
| dc.identifier.issn | 0454-7837 | - |
| dc.identifier.uri | http://hdl.handle.net/2433/178546 | - |
| dc.description.abstract | Analysis of the zonal wind averaged longitudinally is made at 10 mb, 30 mb and 50 mb surfaces for July, August and September 1965, and the results show that the fall reversal of the stratospheric circulations starts at 50 mb near 60°N, and then progresses upwards and south- and northwards. This fact is also confirmed for 6 years from 1957 through 1962. Some discussions are given about the mechanism of this reversal. | en |
| dc.format.mimetype | application/pdf | - |
| dc.language.iso | eng | - |
| dc.publisher | Geophysical Institute, Kyoto University | en |
| dc.subject.ndc | 450 | - |
| dc.title | FALL REVERSAL OF THE LOWER-AND MIDDLE-STRATOSPHERE CIRCULATION IN THE NORTHERN HEMISPHERE | 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 | 7 | - |
| dc.identifier.spage | 45 | - |
| dc.identifier.epage | 56 | - |
| dc.textversion | publisher | - |
| dc.sortkey | 08 | - |
| dcterms.accessRights | open access | - |
| dc.identifier.pissn | 0454-7837 | - |
| 出現コレクション: | No.7 | |
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