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突如其来的波林格-阿勒罗德前变暖和深海循环变化
Nivedita Thiagarajan1, Adam V Subhas1, John R Southon2
1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, USA.
Nature
|July 4, 2014
概括
深海的热量释放引发了北半球突然变暖和大西洋循环在最后一次脱冰期间重新启动. 这一发现重新塑造了我们对过去气候动态和海洋气候反的理解.
科学领域:
- 古海洋学是古海洋学.
- 气候科学 气候科学
- 海洋地质学海洋地质学
背景情况:
- 最后一次脱冰带来了快速的气候变化,包括北半球变暖和海洋循环的变化,但它们的原因仍在争论中.
- 波林-阿勒罗德变暖和大西洋南部翻转循环 (AMOC) 重启是关键事件,但它们的触发因素尚未完全理解.
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