长树环时间表中的低频信号用于重建过去的温度变化
Jan Esper1, Edward R Cook, Fritz H Schweingruber
1Swiss Federal Research Institute WSL, Zuercherstrasse 111, 8903 Birmensdorf, Switzerland.
概括
长树环记录对于了解过去的气候变化和中世纪温暖时期 (MWP) 至关重要. 我们的研究表明,北半球树环数据可以保存多个世纪的温度趋势,支持MWP.
科学领域:
- 古气候学 古气候学
- 气候科学 气候科学
- 登德罗年代学 登德罗年代学
背景情况:
- 准确地重建过去的气候变化对于了解长期温度趋势至关重要.
- 中世纪温暖时期 (MWP) 和20世纪的变暖需要强大的,长期的气候记录进行比较.
- 树环时间表为重建过去的气候条件提供了有价值的代理.
研究的目的:
- 为了证明北半球外热带树环时间表在保护多个世纪的气候变化方面的能力.
- 验证使用树环数据来重建过去1000年的温度趋势.
- 用树环证据评估中世纪温暖时期的大规模发生情况.
主要方法:
- 从北半球外热带地区选取了14个高质量的树环时间表.
- 应用适当的分析方法来保持大规模的,多个世纪的温度趋势.
- 平均选定的时间表来创建一个复合记录.
主要成果:
- 精心挑选的树环时间表可以保持连贯的,大规模的,多世纪的温度趋势.
- 开发的方法确保树环数据中保持关键气候变异性.
- 复合树环记录支持中世纪温暖时期在北半球外热带地区的发生.
结论:
- 树环记录是重建过去在多个世纪的时间尺度上的温度变化的一个可靠来源.
- 这项研究验证了使用树环数据来理解像MWP这样的历史气候事件.
- 这些发现支持中世纪温暖时期在北半球极热带地区的大规模性质.
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