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Updated: May 22, 2026

Evolution of Staircase Structures in Diffusive Convection
07:28

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Published on: September 5, 2018

ホロセーン時代を通して南向きの熱帯間の収束地帯の移動

G H Haug1, K A Hughen, D M Sigman

  • 1Department of Earth Sciences, Eidgenössische Technische Hochschule-Zentrum, CH-8092 Zürich, Switzerland.

Science (New York, N.Y.)
|August 18, 2001
PubMed
まとめ

カリアコ盆地からのチタンと鉄のデータは,南米の降雨の変化の14,000年を示しています. 大西洋熱帯間収束地帯 (ITCZ) と関連したこれらのシフトは,より乾燥した期間と地球的な気候のつながりを示しています.

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