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福岡平野・筑紫平野における夏季晴天時地上風の統計的解析による局地気象の研究
http://hdl.handle.net/10780/781
http://hdl.handle.net/10780/7814d005516-a724-4d9b-a99d-630768b59a49
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
3005_Ueno_Tohjo.pdf (2.1 MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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| 公開日 | 2009-04-16 | |||||
| タイトル | ||||||
| タイトル | 福岡平野・筑紫平野における夏季晴天時地上風の統計的解析による局地気象の研究 | |||||
| 言語 | ja | |||||
| タイトル | ||||||
| タイトル | フクオカ ヘイヤ チクシ ヘイヤ ニ オケル カキ セイテンジ チジョウフウ ノ トウケイテキ カイセキ ニ ヨル キョクチ キショウ ノ ケンキュウ | |||||
| 言語 | ja-Kana | |||||
| タイトル | ||||||
| タイトル | Statistical analysis of surface wind in local meteorology of the Fukuoka and Chikushi Plains | |||||
| 言語 | en | |||||
| 言語 | ||||||
| 言語 | jpn | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | ETYP:教育関連論文 | |||||
| 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 | |||||
| アクセス権 | ||||||
| アクセス権 | open access | |||||
| アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||
| 著者 |
上野, 悠大
× 上野, 悠大× 棟上, 俊二 |
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| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | Surface wind data in fair summer day are statistically analyzed for the purpose to characterize local meteorology in the Fukuoka-Chikushi plane area. Topology of the studied area is similar in environment to Kanto plane or the Nobi plane, like as faced to two different waters. Available data sources, e.g. the JMA's AmeDAS and NIES's AEROS are extracted and used for analysis. 165 fair days are selected from 620 days in summer season on the basis of sunshine hours (more than 6 hours/day). The weather charts are also verified to reject the synoptic scale turbulence, and 108 days are selected as a result. The gridded wind wind profiles are calculated with objective analysis, and also studied the intensity of divergence to estimate the rising air flow. The contour diagram of these divergences show that the Sefuri-mountains and Chikushino-Dazaifu area are obviously strong. This is concordant to high value of SPM amount in Dazaifu area on the analyzed days. This is apparently caused by strengthened thermal by the interaction of two system of sea wind from the Hakata Bay and Ariake Sea. It is possibly predicted the cloud formation by existence of the thermal, enough amount of SPM as condensation nuclei, and humidity in these sea wind. | |||||
| 書誌情報 |
福岡教育大学紀要. 第三分冊, 数学・理科・技術科編 Bulletin of Fukuoka University of Education. Part III, Mathematics, natural sciences and technology 巻 58, p. 89-99, 発行日 2009-02-10 |
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| ISSN | ||||||
| 収録物識別子タイプ | PISSN | |||||
| 収録物識別子 | 0532-811X | |||||
| 出版者 | ||||||
| 出版者 | 福岡教育大学 | |||||
