相关实验视频
Updated: Apr 10, 2026

Using Generative Art to Convey Past and Future Climate Transitions
Published on: March 31, 2023
在最后一个冰河间的海平面上控制双极波
G Marino1, E J Rohling2, L Rodríguez-Sanz1
1Research School of Earth Sciences, The Australian National University, Canberra, Australian Capital Territory 2601, Australia.
最后一个前期的冰川终结 (T-II) 导致海平面迅速上升,与北大西洋寒冷事件Heinrich Stadial 11 (HS11) 有关. 这与最后一个冰川 - 冰川间过渡 (T-I) 相反,表明不同的冰川时代结束过程.
科学领域:
- 古气候学 古气候学
- 海洋学 海洋学 海洋学
- 冰川学的冰川学
背景情况:
- 了解冰河期的终结对于预测未来的气候变化至关重要.
- 目前的模型严重依赖于最后一个冰川-冰川间过渡 (终结I),但它的代表性是不确定的.
- 对于以前的终止,如终止II,需要详细的时间表,以便进行可靠的比较.
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