Synchronous Td'-derived SSTs (.DEG.C.) off Japan with Climatic Events in the Northern Hemisphere
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- KOIZUMI Itaru
- Emeritus Professor of Hokkaido University
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- SAKAMOTO Tatsuhiko
- Japan Agency for Marine-Earth Science and Technology
Bibliographic Information
- Other Title
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- 日本近海の海水温変動と北半球気候変動との共時性
- ニホン キンカイ ノ カイスイオン ヘンドウ ト キタハンキュウ キコウ ヘンドウ ト ノ キョウジセイ
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Abstract
Annual sea-surface temperatures (SSTs) (°C) were derived from a regression analysis between the ratio of warm- and cold-water diatoms (Td' ratio) in 123 surface sediment samples around the Japanese Islands and measured mean annual SSTs (°C) at the core sites. The cross spectra between the atmospheric residual 14C (‰), and annual SSTs (°C) of cores DGC-6 (Japan Sea) and MD01-2421 (off Kashima), respectively, consist of five dominant periods: 6000, 2400, 1600, 950, and 700 years.<br> The amplitude of fluctuations of annual SSTs (°C) in the millennial time scale during the Holocene after the Younger Dryas is within 6-10°C. Periodic variations of annual SSTs (°C) can be correlated within error to abrupt climatic events reported from different paleoclimatic proxy records in many regions of the Northern Hemisphere. The cooling time of annual SSTs (°C) also corresponds to the triple events of high 14C values in the atmospheric residual 14C records, as well as the Bond events in the North Atlantic.
Journal
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- Journal of Geography (Chigaku Zasshi)
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Journal of Geography (Chigaku Zasshi) 119 (3), 489-509, 2010
Tokyo Geographical Society
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Details 詳細情報について
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- CRID
- 1390282679205750912
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- NII Article ID
- 10030369415
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- NII Book ID
- AN00322536
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- ISSN
- 18840884
- 0022135X
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- NDL BIB ID
- 10757682
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- Text Lang
- ja
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- Data Source
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- JaLC
- NDL
- Crossref
- CiNii Articles
- KAKEN
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- Abstract License Flag
- Disallowed