西伯利亚树环中的双碳和氧同位素作为千年阳光持续时间变化的指标
Olga V Churakova Sidorova1, Rolf T W Siegwolf1, Mikhail S Zharkov2
1Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Zürcherstrasse 111, CH-8903 Birmensdorf, Switzerland.
The Science of the total environment
|March 30, 2024
概括
这项研究使用西伯利亚树木环重建了1505年的7月阳光持续时间. 结果显示了显著的变化,包括中世纪的最大值和火山爆发对阳光持续时间的影响.
科学领域:
- 古气候学 古气候学
- 气候科学 气候科学
- 同位素地球化学 同位素地球化学
背景情况:
- 缺乏关于过去夏季阳光持续时间的每年解决的古气候数据,阻碍了对气候系统的理解和建模.
- 西伯利亚的树环为重建过去的阳光持续时间变化提供了潜在的档案.
研究的目的:
- 用树环同位素重建过去1505年的7月阳光持续时间变化.
- 调查阳光持续时间和主要气候驱动因素 (如火山爆发和太阳活动) 之间的关系.
主要方法:
- 使用来自西伯利亚树木环的碳和氧同位素的组合.
- 开发了7月阳光持续时间 (1,5K-SIB-JSDR) 的年度1505年重建.
- 分析了重建与火山事件,大太阳最小值和太阳活动的相关性.
主要成果:
- 与1505年的平均值相比,中世纪时期的7月阳光持续时间比1505年的平均值高56%.
- 在主要的平流层火山爆发后,观察到阳光持续时间的显著减少 (高达60%).
- 重建成功保存了太阳极小期的信号和太阳黑子总数.
结论:
- 西伯利亚树环同位素为重建过去夏季阳光持续时间提供了强大的代理.
- 1,5K-SIB-JSDR重建显示了与火山活动和太阳周期有关的显著气候变化.
- 这项研究强调了大规模气候信号保留在阳光持续时间重建中的潜力.
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