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氧-18同位素组成,降水和气候的长期趋势之间的关系
概括
降水中的稳定同位素比率是古气候的关键指标. 这项研究显示了降水量.
科学领域:
- 古气候学 古气候学
- 同位素水文学 同位素水文学
- 气候科学 气候科学
背景情况:
- 水中氧 (18O/16O) 和 (D/H) 的稳定同位素比例是重要的古气候代理.
- 古气候数据的定量解释受到全球同位素行为的不完全理解的限制.
研究的目的:
- 为了研究降水的同位素组成和表面空气温度之间的关系.
- 分析中高度地区的同位素组成和温度的长期趋势.
主要方法:
- 来自IAEA-WMO"降水中的同位素"网络的月度降水和地表空气温度数据的分析.
- 在过去的三十年里,对氧-18含量 (delta 18O) 和温度进行时间序列分析.
主要成果:
- 长期降水同位素组成的变化密切跟踪了表面空气温度的变化.
- 确定了大约0.6每毫米每摄氏度的平均18O温度系数.
结论:
- 强烈的相关性支持使用降水的同位素组成作为可靠的古气候指标.
- 提供了从古气候同位素记录中重建过去温度的定量关系.
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