来自斐济的Coral Sr/Ca-SST重建延伸到公元1370年,揭示了对十年间太平洋振荡的洞察力
Juan P D'Olivo1,2,3, Jens Zinke4,5,6, Rishav Goyal7,8
1Unidad Académica de Sistemas Arrecifales, Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Puerto Morelos 77580, Mexico.
Science advances
|August 14, 2024
概括
一个627年的珊瑚记录揭示了十年间太平洋振荡 (IPO) 影响太平洋气候. 20世纪出现了不寻常的变暖和微弱的坡度,影响了降雨量,并可能使珊瑚海地区干.
科学领域:
- 古气候学 古气候学
- 气候动力学 气候动力学
- 海洋学 海洋学 海洋学
背景情况:
- 十年间太平洋振荡 (IPO) 是全球气候变化的主要驱动因素.
- 西南热带太平洋是IPO动态的关键地区.
- 了解长期IPO变化对于预测未来气候趋势至关重要.
研究的目的:
- 来自斐济的627年海面温度 (SST) 记录的重建,作为IPO西南极的代理.
- 通过重建西南和中太平洋 (SWCP) 之间的SST梯度来开发IPO波动的可靠代理.
- 分析百年级温度趋势及其对整个太平洋气候远程连接的影响.
主要方法:
- 珊瑚 Sr/Ca 地化学重建过去的海面温度.
- 一个新的627年斐济珊瑚记录与现有的古气候数据的整合.
- 分析西南和中部太平洋 (SWCP) 之间的海面温度梯度作为IPO代理.
- 与气候模型模拟进行比较,以了解IPO的影响.
主要成果:
- 来自斐济的627年的珊瑚基SST重建提供了IPO西南极的详细历史.
- 重建的SWCP梯度揭示了过去六个世纪的明显的百年级温度趋势.
- 20世纪的条件呈现出前所未有的盆地规模的变暖,与前几个世纪相比,区域-南部梯度减弱.
- 软弱的SWCP梯度显著影响了赤道太平洋的IPO相关降雨模式.
- 西部和中部太平洋地区持续的同步变暖可能导致珊瑚海地区的干旱.
结论:
- 该研究提供了SWCP梯度的最长的珊瑚基重建,为IPO变化提供了新的见解.
- 20世纪代表了远离长期IPO行为,对区域气候产生影响.
- 预计珊瑚海地区的干燥趋势对太平洋岛国构成风险,原因是IPO动态发生了变化.
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