在过去的80万年中,大气中CH4的轨道和千年规模的特征
Laetitia Loulergue1, Adrian Schilt, Renato Spahni
1Laboratoire de Glaciologie et Géophysique de l'Environnement, CNRS-Université Joseph Fourier Grenoble, 54 Rue Molière, 38402 St Martin d'Hères, France.
Nature
|May 16, 2008
概括
大气中的甲含量随着超过80万年的冰川周期而波动. 热带湿地变化和冰盖撤退影响了这些温室气体变化,影响了气候.
科学领域:
- 古气候学 古气候学
- 温室气体动态 温室气体动态
- 冰芯分析 冰芯分析
背景情况:
- 大气中的甲是一种强大的温室气体,对于了解气候变化和过去的温度变化至关重要.
- 从历史上看,甲的度在10亿分之350至800个体积 (p.p.b.v.) 之间. 在冰川和冰川间时期之间.
- 目前的甲含量 (约1,770 p.p.b.v.) 是什么? 远远超过工业化前的范围,需要研究其控制机制.
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