热带太平洋对太阳强迫的动态反应在早期的全新世纪
Thomas M Marchitto1, Raimund Muscheler, Joseph D Ortiz
1Department of Geological Sciences and Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA. tom.marchitto@colorado.edu
概括
这项研究揭示了巴哈加利福尼亚州的Holocene海面温度,显示了与太阳周期和厄尔尼诺-南方振荡 (ENSO) 动态相关的早期温暖. 这些发现提供了对过去气候变化和海洋反应的见解.
科学领域:
- 古代海洋学 古代海洋学 古代海洋学
- 气候科学 气候科学
- 海洋地球化学 海洋地球化学
背景情况:
- 厄尔尼诺-南方振荡 (ENSO) 显著影响巴哈加利福尼亚州海面温度 (SST) 的年间变化.
- 了解过去的ENSO行为及其驱动因素对于预测未来的气候模式至关重要.
研究的目的:
- 为了重建一个高分辨率的Holocene SST记录从巴哈加利福尼亚州南部的西海岸.
- 调查过去的SST,太阳变化和ENSO类条件之间的关系.
主要方法:
- 使用高分辨率的/ (Mg/Ca) 代理来确定过去的海面温度.
- 相关的SST波动与太阳变量的宇宙原核代体.
主要成果:
- 早期到中期的Holocene SSTs更冷,与东方赤道太平洋的冷却和轨道强迫模拟保持一致.
- 早期Holocene的千年级SST波动与太阳最小值相关,表明类似于厄尔尼诺的情况.
- 观察到的模式与理论模式保持一致.
- 海洋动态恒温器海洋动态恒温器
- ENSO对辐射强迫的反应.
结论:
- Mg/Ca代理记录为北太平洋的Holocene海洋大气动力学提供了宝贵的见解.
- 太阳的变化可能影响了ENSO在早期Holocene的行为.
- 这些发现支持ENSO应对外部气候强迫的理论模型.
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