区域气候变化是由平世纪时期全球逐渐冷却引起的
Ana Christina Ravelo1, Dyke H Andreasen, Mitchell Lyle
1Ocean Sciences Department, University of California, Santa Cruz, California 95064, USA. acr@es.ucsc.edu
Nature
|May 21, 2004
概括
地球的气候在400万年间逐渐冷却,这是由逐渐的变化驱动的,而不是单一事件. 低度条件显著影响全球气候反.
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:
- 地球的气候在过去的400万年里从温暖过渡到凉爽.
- 构造学对海洋热传输的影响被认为是这种过渡的原因.
- 全球冷却和冰川的确切驱动因素仍在争论中.
研究的目的:
- 为了调查地球长期气候转型的原因.
- 将不同度的气候记录进行比较,以了解冷却模式.
- 为了确定低度气候和高度气候灵敏度之间的关系.
主要方法:
- 从高度,亚热带和热带地区的气候记录进行比较分析.
- 检查气候冷却时间的区域差异.
- 评估高度气候对太阳能加热变化的敏感性.
主要成果:
- 冰川/间冰川周期的开始并不与单一的低度气候重组一致.
- 全球冷却是一个渐进的过程,而不是突然发生的事件.
- 高度地区的气候敏感性逐渐增加,特别是在200万年前之后.
结论:
- 区域气候差异表明全球逐渐冷却过程.
- 建立了凉爽的热带和亚热带上游条件,先后增加了对高度的敏感性.
- 平均低度气候条件在全球气候反中发挥着重要作用.
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