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中世过渡:对越来越多的积极反的延迟反应?
J D Shackleton1, M J Follows1, P J Thomas2
1Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139 USA.
地球的冰川 - 冰川间周期在普莱斯托时代中期过渡 (MPT) 期间的周期性发生了变化. 这项研究表明,气候系统反的逐渐增加,而不是外部强迫,导致了这一重大气候事件.
科学领域:
- 古气候学 古气候学
- 气候动力学 气候动力学
- 地球系统科学 地球系统科学
背景情况:
- 冰川 - 冰川间周期显示了地球气候的自然变化.
- 中世过渡 (MPT) 标志着主导周期周期从大约4万年到10万年的重大转变.
研究的目的:
- 调查MPT是由气候系统内部周期的增加引起的假设.
- 探索积极反在调节气候周期周期性中的作用.
主要方法:
- 利用碳循环模型,结合化物种群和海洋性之间的反.
- 模拟大气二氧化碳水平及其对气候系统周期性的影响.
主要成果:
- 证明气候系统的内部周期对积极反的强度很敏感.
- 通过碳循环模型成功模拟了类似于MPT的循环周期变化.
- 观察到周期性变化可以在反强度变化数百万年后表现出来.
结论:
- 可能是气候系统反发生在观察到的周期性转移之前很久的变化引发了MPT.
- 气候系统的内部动态,特别是反机制,在长期气候变化中起着至关重要的作用.
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