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1987年に観測された長崎県南部地方の対流性降雨の微細構造
http://hdl.handle.net/10069/32447
http://hdl.handle.net/10069/32447462aef89-6195-49cc-ba31-f39bc630ef78
名前 / ファイル | ライセンス | アクション |
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kyoikuS40_055.pdf (993.2 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2013-06-25 | |||||
タイトル | ||||||
タイトル | 1987年に観測された長崎県南部地方の対流性降雨の微細構造 | |||||
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 |
荒生, 公雄
× 荒生, 公雄× 椿, 隆博× 中田, 勝夫 |
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著者別名 | ||||||
姓名 | Arao, Kimio | |||||
著者別名 | ||||||
姓名 | Tsubaki, Takahiro | |||||
著者別名 | ||||||
姓名 | Nakata, Masao | |||||
その他のタイトル | ||||||
その他のタイトル | Fine Structure of Convective Rainnstorms over Nagasaki in 1987 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The rainfall in 1987 monsoon season over the south of Nagasaki Prefecture was studied with a special interest in the raphic enhencement of convective clounds. The PPI marine radar of 3.2cm wavelength and three rain-guages with a digital printer were the main equipments of this study. The records of 34 rain-gauges of ordinary type in this region were lso utilized for estimating the movement of clound system. The results of this study are summarized as follows: (1) The in-guage with a digital printer, which prints out both the time (hour, minute and second) and the accumurated amount of rainfall for every 0.5mm pulse, is very useful for evaluating the rainfall amount in a short time period such as one, five or ten minutes. (2) The behavior of the thunderstorm on 5 July was very interesting, because the development of this rain system was simliar to that of the Nagasaki heavy rainfall occurred in 1982. New convective rain cells of this storm were generated at the southwestern end of the storm region and moved to the east, so that the orographic effects of Nishisonogi Peninsula is more or less attribtable to the development of the storm. (3) One of the interesting features was the line-shaped rain and with very narrow width and with long life me, which extended from the eastern part of Nagasaki City to Isahaya City. New cells of this system occured the west end of e line. The behavior of this rain cloud also suggests an orographic effect due to the moderate hills of Nagasaki Peninsula. | |||||
書誌情報 |
長崎大学教育学部自然科学研究報告 en : Science bulletin of the Faculty of Education, Nagasaki University 巻 40, p. 55-66, 発行日 1989-02-28 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0386443X | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00178280 | |||||
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 | |||||
論文ID(NAID) | ||||||
関連タイプ | isIdenticalTo | |||||
識別子タイプ | NAID | |||||
関連識別子 | 40002768786 | |||||
出版者 | ||||||
出版者 | 長崎大学教育学部 | |||||
引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 長崎大学教育学部自然科学研究報告. vol.40, p.55-60; 1989 |