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Updated: Jun 20, 2026

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Using Generative Art to Convey Past and Future Climate Transitions
Published on: March 31, 2023
扩大太平洋气候系统对一个小的11年太阳循环的反应,迫使太平洋气候系统对一个小的11年太阳循环的反应
Gerald A Meehl1, Julie M Arblaster, Katja Matthes
1National Center for Atmospheric Research, Post Office Box 3000 Boulder, CO 80307, USA. meehl@ncar.ucar.edu
概括
11年的太阳周期通过平流层臭氧和海洋-大气相互作用影响太平洋气候. 这些联合机制放大了太阳强迫,影响了热带降雨和海面温度.
科学领域:
- 气候科学 气候科学
- 大气科学 大气科学
- 海洋学 海洋学 海洋学
背景情况:
- 太阳的11年周期导致太阳能输出的小变化.
- 在热带太平洋地区观察到的气候信号比从太阳变化中预期的要大.
- 了解将太阳周期与太平洋气候联系在一起的机制至关重要.
研究的目的:
- 研究平流层臭氧和海洋大气相互作用如何影响太平洋气候.
- 确定两种拟议机制对太阳引起的气候信号的综合影响.
- 量化太阳表面强迫的放大.
主要方法:
- 利用了三个全球气候模型.
- 模拟平流层臭氧对太阳强迫的反应 (上下机制).
- 模拟的合海洋 - 大气表面对太阳强迫的反应 (自下而上的机制).
- 分析了模型输出,每个机制单独和共同作用.
主要成果:
- 结合起来,这些机制增加了太平洋的赤道外热带降雨量.
- 东方赤道太平洋海面温度在太阳周期峰值期间下降.
- 降低低度云扩大了表面的太阳力.
结论:
- 平流层和地表气候机制之间的相互作用是理解太阳周期影响的关键.
- 组合的机制显著放大了太阳变化的影响,在热带太平洋.
- 这项研究阐明了太阳周期影响地球气候系统的途径.
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