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  1. 学術雑誌掲載済論文
  2. 洋雑誌

Dating of the Dome Fuji, Antarctica deep ice core (scientific paper)

https://kitami-it.repo.nii.ac.jp/records/7198
3654803a-7eee-42ac-9db5-4aa10bcc567a
名前 / ファイル ライセンス アクション
4430.pdf 4430.pdf (4.5 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2007-06-13
タイトル
言語 en
タイトル Dating of the Dome Fuji, Antarctica deep ice core (scientific paper)
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
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 Watanabe, Okitsugu

× Watanabe, Okitsugu

WEKO 36699

en Watanabe, Okitsugu

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Shoji, Hitoshi

× Shoji, Hitoshi

WEKO 36700

en Shoji, Hitoshi

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Satow, Kazuhide

× Satow, Kazuhide

WEKO 36701

en Satow, Kazuhide

Search repository
Motoyama, Hideaki

× Motoyama, Hideaki

WEKO 36702

en Motoyama, Hideaki

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Fujii, Yoshiyuki

× Fujii, Yoshiyuki

WEKO 36703

en Fujii, Yoshiyuki

Search repository
Narita, Hideki

× Narita, Hideki

WEKO 36704

en Narita, Hideki

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Aoki, Shuji

× Aoki, Shuji

WEKO 36705

en Aoki, Shuji

Search repository
著者別名
姓名
姓名 庄子, 仁
言語 ja
抄録
内容記述タイプ Abstract
内容記述 The Antarctic ice sheet preserves paleo-climate information in the form of physical and chemical stratigraphy. A deep ice core was continuously drilled down to a depth of 2,503 m at Dome Fuji station, East Dronning Maud Land, Antarctica, during the 1993-97 JARE inland operations. Oxygen isotope measurements were conducted on 7 to 50 cm-long ice core samples selected from the entire core depth. A time scale for the Dome Fuji core is calculated from past accumulation rates and an ice flow model. Past accumulation rates were converted from oxygen isotope values by using an empirical equation obtained in the Dome Fuji area. A steady-state flow model was preciously developed for a time scale calculation of the Summit ice core, Greenland. Using reference depth points from volcanic signals and annual layer thickness values measured on the Dome Fuji core allows for tuning of the calculated time scale. A depth-age profile was obtained for the past 320 kyr. The obtained paleo-temperature profile shows the characteristics of the past three glacial and interglacial periods. The power spectrum of δ^<18>O change over an interval of 320 kyr reveals three dominant cycles. The paleo-temperature profile coincides quite well with the Vostok ice core data in general but not in detail, suggesting that further studies are needed both for chronological investigations and a multi-factor, cross-correlation analysis between deep ice cores for climatological understanding.
書誌情報 Memoirs of National Institute of Polar Research, Special Issue

巻 57, p. 25-37, 発行日 2003-03
権利
権利情報 NATIONAL INSTITUTE OF POLAR RESEARCH, O.Watanabe, H.Shoji, K.Satow, H.Motoyama, Y.Fujii, H.Narita, S.Aoki, Memoirs of National Institute of Polar Research. Special issue, 57, 2003, 25-37
フォーマット
内容記述タイプ Other
内容記述 application/pdf
出版者
出版者 国立極地研究所
著者版フラグ
値 publisher
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
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