WEKO3
アイテム
上層低気圧の一例
http://hdl.handle.net/10131/2874
http://hdl.handle.net/10131/28749383dd80-3382-4f98-a7b1-d90ab1915287
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
KJ00004479185.pdf (720.9 kB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2007-09-27 | |||||
| タイトル | ||||||
| タイトル | 上層低気圧の一例 | |||||
| 言語 | ||||||
| 言語 | jpn | |||||
| 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 | |||||
| 著者 |
増井, 次夫
× 増井, 次夫 |
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| 著者(ヨミ) | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 7215 | |||||
| 姓名 | マスイ, ツギオ | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 7216 | |||||
| 姓名 | Masui, Tsugio | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | The high level cyclone which moved over the Central Japan on March 24-25, 1952 was a particular case with remarkable characteristics in the Far East for the period 1951 to 1957. This high level cyclone appeared near the Taimyr Peninsula on March 21 and moved rapidly southeastward across Siberia and Manchuria. On March 24 when this cyclone progressed into the Sea of Japan its shape was elongated in the direction of the movement and the whole area was divided into two parts. The coldest part on 500mb surface, namely the main center of the high level cyclone, was located on the rear side. This center crossed the Central Japan on March 24-25 and the southernmost position of its track reached as low as 34°N and then it turned to northeastward. The most remarkable features appearing on the vertical cross section of this cyclone, compared with the Palmen's cutoff cyclone model, are as follows: 1. The features on the vertical cross section are not symmetric and the axis of warm air column in upper layer tilts northeastward. 2. The cold dome is distinct inspite of its small scale. 3. In the central portion the tropopause is very low (descending to near 500mb surface) and in the stratosphere air temperature is very high compared with ordinary high level cyclones. 4. Many surface cyclones steered by this high level cyclone are formed successively and among them the fourth surface cyclone is formed suddenly off the South-East Coast of the Central Japan. When the high level cyclone moves into North Pacific Ocean, only this surface cyclone develops. | |||||
| 書誌情報 |
横浜国立大学理科紀要. 第一類, 数学・物理学 巻 7, p. 29-43, 発行日 1958-09-30 |
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| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 00858366 | |||||
| 書誌レコードID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AN00408959 | |||||
| フォーマット | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | application/pdf | |||||
| 著者版フラグ | ||||||
| 出版タイプ | VoR | |||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
| その他のタイトル | ||||||
| その他のタイトル | A Case Study of High Level Cyclone | |||||
| 出版者 | ||||||
| 出版者 | 横浜国立大学 | |||||
