双极影响和海因里希型气候变化的阶段化
Kaden C Martin1, Christo Buizert2, Jon S Edwards2
1College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR, USA. martkade@oregonstate.edu.
Nature
|April 24, 2023
概括
海因里希事件与冰盖融水脉冲有关, 并没有冷却格陵兰, 而是导致南极变暖. 这表明海洋远程连接在这些极端的冰河时代事件中影响了气候.
科学领域:
- 古气候学
- 冰盖动力学
- 气候远程连接
背景情况:
- 海因里希事件是冰山在冰河时代从劳伦蒂冰层排放的极端事件.
- 这些事件对全球水文和生态化学循环产生了重大影响.
- 之前的研究很难将海因里希事件与格陵兰的温度联系起来,
研究的目的:
- 调查海因里希事件对格陵兰和南极地区的气候影响.
- 确定海因里希事件相对于南极气候变化的分阶段.
- 了解在这些事件中导致气候变化的远程连接.
主要方法:
- 用格陵兰冰核稳定的同位素作为温度代理的分析.
- 对南极冰核进行温度和甲记录的检查.
- 格陵兰和南极气候信号在海因里希运动场期间的比较.
主要成果:
- 海因里希事件对格陵兰没有可检测的温度影响;在一些海因里希事件开始时发生了冷却.
- 南极冰芯显示了海因里希事件中甲增加的加速变暖.
- 南极的变暖使得格陵兰的变冷时间大约落后了133年,
结论:
- 尽管没有直接的格陵兰温度信号,但海因里希事件对南极气候的影响比格陵兰气候更大.
- 海洋远程连接可能是海因里希事件的气候影响的媒介,将北大西洋冰流与南半球变暖联系起来.
- 亨利希事件的复杂空间动态表明局部冲击和远程放大.
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