阳光照射驱动的10万年冰川周期和冰盖体积的歇斯底里
Ayako Abe-Ouchi1, Fuyuki Saito, Kenji Kawamura
1Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa 277-8568, Japan. abeouchi@aori.u-tokyo.ac.jp
Nature
|August 9, 2013
概括
北半球的冰盖表现出由阳光和内部反驱动的10万年周期. 冰盖对阳光照射的反应中的歇斯底里解释了冰川周期的逐渐增长和快速撤退特征.
科学领域:
- 古气候学 古气候学
- 冰川学的冰川学
- 气候建模气候模型
背景情况:
- 北半球的冰盖显示了一个10万年周期,逐渐增长和快速终结.
- 米兰科维奇理论将冰川周期与轨道周期联系起来,但仅靠阳光照射并不能解释10万年周期.
研究的目的:
- 研究冰川周期的10万年周期背后的机制.
- 解释内部反在冰盖动态中的作用.
主要方法:
- 使用了全面的气候和冰盖模型.
- 分析了冰盖对夏季阳光照射的歇斯底里反应.
主要成果:
- 阳光照射与气候,冰盖和石化层-石化层反相结合,解释了10万年周期.
- 冰盖平衡状态显示歇斯底里,影响冰川周期周期.
- 延迟的静态反弹有助于快速的冰盖撤退.
结论:
- 10万年冰川周期是由阳光和内部反的组合驱动的.
- 冰盖行为的歇斯底里对于理解冰川终结至关重要.
- 虽然二氧化碳起到作用,但它不是这些长期循环的主要驱动因素.
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