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「中世温暖期(MCA)」と9世紀末の気候的不安定について
https://doi.org/10.15099/00000826
https://doi.org/10.15099/0000082678378862-7e13-4977-a192-3c73a072a131
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
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公開日 | 2013-03-11 | |||||||
タイトル | ||||||||
タイトル | 「中世温暖期(MCA)」と9世紀末の気候的不安定について | |||||||
言語 | ||||||||
言語 | jpn | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | 気候変動 | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | 中世温暖期 | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | 祈雨 | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | 干ばつ | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | Climate Change | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | Medieval Climate Anomaly | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | Pray for rain | |||||||
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 | |||||||
ID登録 | ||||||||
ID登録 | 10.15099/00000826 | |||||||
ID登録タイプ | JaLC | |||||||
著者 |
田上, 善夫
× 田上, 善夫
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著者別名 | ||||||||
姓名 | TAGAMI, Yoshio | |||||||
その他(別言語等)のタイトル | ||||||||
その他のタイトル | On the "Medieval Climate Anomaly" and climate instability around the end of 9th century | |||||||
抄録 | ||||||||
内容記述タイプ | Abstract | |||||||
内容記述 | In this study, reconstruction of MCA (Medieval Climate Anomaly) through proxy data was tried to clarify its nature. At first, "prayers for rain" records were collected from "Rikkokushi", six national histories of the ancient Japan, and the climate variation was clarified by their appearance changes. Next, the climate variation of Japan was compared with those from MCAreconstruction studies on many areas in the world. Furthermore, MCA was examined by comparison with its simulation by global circulation model. The main results are as follows: 1) There remain many records on prayers for rain from the end of the first millennium to the beginning of the second millennium, which may show that it was time of warm and dry climate condition. 2) During MCA, there might have been a period of cool and moist condition around 900, specifically from 880 to 910. 3) A prevailing circulation like La Nina on the Pacific Ocean played an important role in MCA. 4) Around the Atlantic Ocean, the North Atlantic Oscillation was usually at its positive mode, and played an important role for the climate there. | |||||||
引用 | ||||||||
内容記述タイプ | Other | |||||||
内容記述 | 富山大学人間発達科学部紀要, 7巻1号, Page 91-105 | |||||||
書誌情報 |
富山大学人間発達科学部紀要 巻 7, 号 1, p. 91-105, 発行日 2012-10-25 |
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ISSN | ||||||||
収録物識別子タイプ | ISSN | |||||||
収録物識別子 | 1881316X | |||||||
書誌レコードID | ||||||||
収録物識別子タイプ | NCID | |||||||
収録物識別子 | AA12181167 | |||||||
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 | |||||||
出版者 | ||||||||
出版者 | 富山大学人間発達科学部 | |||||||
資源タイプ(DSpace) | ||||||||
内容記述タイプ | Other | |||||||
内容記述 | Article |