热环循环中的短路:北半球冰期的原因?
1N. W. Driscoll, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. G. H. Haug, GEOMAR, Forschungszentrum fur Marine Geowissenschaften, Universitat Kiel, Wischhofstrasse 1-3, D-24148 Kiel, Germany.
概括
北半球冰川形成的原因仍然不确定. 加强西伯利亚河流向北极的淡水输送可能通过增加白度和减少海洋热传输来促进冰的形成.
科学领域:
- 地球科学 地球科学 地球科学
- 古气候学 古气候学
- 海洋学 海洋学 海洋学
背景情况:
- 普世-普世过渡期 (约300万年前) 见证了北半球冰期的开始,这是一个主要的气候变化.
- 巴拿马峡的关闭是拟议的驱动因素,增强了海洋循环和高度湿度,但可能会因热传输增加而抑制冰的生长.
研究的目的:
- 调查北半球冰川的潜在机制,调和增加湿度和热传输的影响.
主要方法:
- 这项研究提出了一个基于现有的古海洋学和气候模型的假设.
- 它的重点是淡水排放到北冰洋的作用.
主要成果:
- 通过加强大气循环向欧亚大陆增强的水分传输可以增加通过西伯利亚河流向北冰洋排放的淡水.
- 这种淡水的涌入可以促进海冰的形成,从而增加行星的白度.
- 增加的海冰覆盖将隔离海洋,减少热量转移到大气层,并抵消全球变暖的影响.
结论:
- 通过西伯利亚河流向北极提供淡水供应,为启动北半球冰川形成提供了一个合理的机制.
- 这一过程涉及一个负反循环,其中增加的冰盖减少了海洋和大气的热交换,促进了进一步的冷却和冰的增长.
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