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由海底分布形成的深海翻转
C de Lavergne1,2, G Madec2, F Roquet3
1School of Mathematics and Statistics, University of New South Wales, Sydney, New South Wales 2052, Australia.
Nature
|November 10, 2017
概括
的海洋
科学领域:
- 海洋学
- 气候科学
- 地质学
背景情况:
- 对于全球的热量和碳储存至关重要.
- 对于了解长期气候调节来说, 深海翻流的强度和结构至关重要.
研究的目的:
- 调查深翻转循环强度和结构的控制因素.
- 确定海底地形如何影响半球间的水质运输.
主要方法:
- 在南32度以北的海底深度分布分析.
- 历史放射性碳测量的解释.
- 对深水流模式的建模.
主要成果:
- 南32度以北的海底地形将密集的南方源水向北导向4公里以下.
- 这些水的回流主要发生在2.5公里以上.
- 中间深度 (1-2.5公里) 显示没有北方通风的弱中午流.
结论:
- 海洋盆地几何学显著限制了深海翻转循环.
- 海底地形是深海水体路径和储存的主要驱动因素.
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