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热带山脉冰芯 δ18 O:全球气温变化的金髮女孩指标
Zhengyu Liu1,2,3, Yuntao Bao1, Lonnie G Thompson3,4
1Department of Geography, Ohio State University, Columbus, OH, USA.
热带阿尔卑斯山冰芯揭示了过去的气候变化. 稳定的水氧同位素 (δ18Oice) 表示中/上热层温度和冰川时期的全球冷却.
科学领域:
- 古气候学 古气候学
- 气候建模气候模型
- 冰川学的冰川学
背景情况:
- 热带阿尔卑斯山冰芯为上层大气提供了宝贵的古气候数据.
- 将稳定的水氧同位素比率 (δ18Oice) 解释为气候代理是具有挑战性的.
研究的目的:
- 为了澄清热带冰芯稳定水氧同位素 (δ18O冰) 的气候解释.
- 建立 δ 18 O 冰作为中上热带层温度和全球平均表面温度变化的指标.
主要方法:
- 整合来自冰芯的代理记录.
- 利用气候模型和现代卫星测量.
- 辐射-对流平衡理论的应用.
主要成果:
- 热带 δ18 冰精确地反映了中部和上部热带层的温度.
- 在中/上热带层估计的冰川冷却: -7.35° ± 1.1°C.
- 提供了全球平均表面在冰川阶段冷却的独立估计: -5.9° ± 1.2°C.
结论:
- 热带冰核中稳定的水氧同位素是过去大气温度的可靠代理.
- 这项研究提供了一种新的,与海洋无关的方法来估计冰川的冷却.
- 综合所有数据,冰川冷却的最大概率估计为-5.85° ± 0.51°C.
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