General tendencies of stable isotopes and major chemical constituents of the Dome Fuji deep ice core (scientific paper)

Stable isotope compositions of water and major chemical constituents of the Dome Fuji ice core are analyzed and the data sets over the entire depth of the 2503-m core are presented in appropriate time resolution as consecutive series of average value in definite terms. These results based on the fir...

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Bibliographic Details
Main Authors: Okitsusgu Watanabe, Kokichi Kamiyama, Hideaki Motoyama, Yoshiyuki Fujii, Makoto Igarashi, Teruo Furukawa, Kumiko Goto-Azuma, Takashi Saito, Satoru Kanamori, Nobuko Kanamori, Naohiro Yoshida, Ryu Uemura
Format: Report
Language:English
Published: National Institute of Polar Research/National Institute of Polar Research/National Institute of Polar Research/National Institute of Polar Research/National Institute of Polar Research/National Institute of Polar Research/National Institute of Polar Research/Disaster Prevention Research Institute, Kyoto University/National Institute of Polar Research/National Institute of Polar Research/Tokyo Institute of Technology/Tokyo Institute of Technology 2003
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Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2459
http://id.nii.ac.jp/1291/00002459/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2459&item_no=1&attribute_id=18&file_no=1
Description
Summary:Stable isotope compositions of water and major chemical constituents of the Dome Fuji ice core are analyzed and the data sets over the entire depth of the 2503-m core are presented in appropriate time resolution as consecutive series of average value in definite terms. These results based on the first stage analyses allow a temporal climatic dividing of the three glacial-interglacial cycles present in the records. A Comparison of the climatic and environmental characteristics of these climate stages is presented.