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Updated: May 13, 2026
07:28
Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
スノーボルのダイナミクス 地球の海洋 地球の海洋
Yosef Ashkenazy1, Hezi Gildor, Martin Losch
1Department of Solar Energy and Environmental Physics, The Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Midreshet Ben-Gurion, 84990, Israel. ashkena@bgu.ac.il
Nature
|March 8, 2013
まとめ
ネオプロテロゾイク期のスノーボール地球は,以前の仮定に反して,活発な循環を持つダイナミックでよく混合された海洋を持っていたかもしれません. この海洋のダイナミクスは,地球規模の氷河期における融解速度と光合成生命の生存に影響を与えた.
科学分野:
- 古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは
- 海洋学 海洋学 海洋学
- 地質物理学 地質物理学とは地質物理学です.
背景:
- スノーボール・アース仮説は,ネオプロテロゾーイク時代に,地球全体で氷河が覆われた惑星を提案している.
- 海洋のダイナミクスを理解することは,地質学的証拠を解釈し,これらの極端な気候の間に生命の生存を評価するために不可欠です.
関連する概念動画
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02:06Conditions on Early Earth
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