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Updated: Jun 25, 2026

Evolution of Staircase Structures in Diffusive Convection
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熱帯太平洋におけるプレイストセンの中期への移行

Martín Medina-Elizalde1, David W Lea

  • 1Department of Earth Science, University of California Santa Barbara, Santa Barbara, CA 93106-9630, USA.

Science (New York, N.Y.)
|October 15, 2005
PubMed
まとめ

プレイストセーン中期の気候の変化は,海面温度 (SST) の振動が41,000年周期から100,000年周期に変化していることを示しています. これらの熱帯太平洋のSSTの変化は,氷の体積の変化に先行し,大気中の二酸化炭素が重要な要因であると示唆しています.

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