Equatorward shift of the subarctic boundary in the northwestern Pacific during the last deglaciation
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- Masanobu Yamamoto
- Graduate School of Environmental Earth Science Hokkaido University Sapporo Japan
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- Ryutaro Suemune
- Graduate School of Environmental Earth Science Hokkaido University Sapporo Japan
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- Tadamichi Oba
- Graduate School of Environmental Earth Science Hokkaido University Sapporo Japan
書誌事項
- 公開日
- 2005-03
- 権利情報
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- http://onlinelibrary.wiley.com/termsAndConditions#vor
- DOI
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- 10.1029/2004gl021903
- 公開者
- American Geophysical Union (AGU)
この論文をさがす
説明
<jats:p>We have generated a high‐resolution record of alkenone sea surface temperature (SST) between 10–24 ka from Core MD01‐2421 off central Japan, in the northwestern Pacific. The cooling by 5°C from 21 ka to 12.8 ka implies the equatorward shift of the subarctic boundary in the northwestern Pacific by ∼2.8° in latitude. This shift was a result of the stronger summer Okhotsk High. The Okhotsk High was likely enhanced by the combined effects of El Niño‐like conditions in the tropical Pacific and the heating of the land surface of northeastern Siberia.</jats:p>
収録刊行物
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- Geophysical Research Letters
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Geophysical Research Letters 32 (5), L05609-, 2005-03
American Geophysical Union (AGU)
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キーワード
詳細情報 詳細情報について
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- CRID
- 1361699995047697536
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- ISSN
- 19448007
- 00948276
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- HANDLE
- 2115/28772
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- データソース種別
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- Crossref
- OpenAIRE
