WEKO3
アイテム
Frontogenesis and frontolysis of the subpolar front in the surface mixed layer of the Japan Sea
http://hdl.handle.net/10069/34415
http://hdl.handle.net/10069/34415b2dda275-4f6a-4602-a554-dc12a7490b2a
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
JGRO119_1498.pdf (7.5 MB)
|
|
| Item type | 学術雑誌論文 / Journal Article(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2014-09-01 | |||||
| タイトル | ||||||
| タイトル | Frontogenesis and frontolysis of the subpolar front in the surface mixed layer of the Japan Sea | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | frontogenesis | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | frontolysis | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | subpolar front | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | the Japan Sea | |||||
| 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 | journal article | |||||
| 著者 |
Zhao, Ning
× Zhao, Ning× Manda, Atsuyoshi× Han, Zhen |
|||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | The frontogenesis and frontolysis processes of the subpolar front (SPF) in the surface mixed layer of the Japan Sea are investigated using state-of-the-art oceanic reanalysis data. The SPF experiences a 9 month weakening period from January to September, which shifts to a strengthening period in October. Our analysis shows that horizontal advection consistently contributes to the intensification of the SPF. After September, as the weakening effect of surface heat flux diminishes, horizontal advection becomes the dominant factor that contributes to changes in the SPF strength. Thus, the SPF enters a 3 month strengthening period. The geostrophic component of horizontal advection provides the most important contribution to strengthening the SPF, acting to intensify the SPF year-round. Ekman advection also promotes SPF strengthening with a smaller but still important contribution. During the weakening period, SPF strength is largely controlled by heat flux. The heat flux, especially the shortwave radiation component, is the primary cause of the surface front disappearance in the summer. | |||||
| 書誌情報 |
Journal of Geophysical Research: Oceans 巻 119, 号 2, p. 1498-1509, 発行日 2014-02 |
|||||
| 出版者 | ||||||
| 出版者 | American Geophysical Union | |||||
| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 21699275 | |||||
| DOI | ||||||
| 関連タイプ | isIdenticalTo | |||||
| 識別子タイプ | DOI | |||||
| 関連識別子 | 10.1002/2013JC009419 | |||||
| 権利 | ||||||
| 権利情報 | c 2014. American Geophysical Union. All Rights Reserved. | |||||
| 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 | |||||
| 引用 | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | Journal of Geophysical Research: Oceans, 119(2), pp.1498-1509; 2014 | |||||
