地磁场与气候相关性研究五十年  

Fifty-year investigation of the correlation between the geomagnetic field and climate

作　　者：王誉棋 何飞 魏勇[1,2] 戎昭金 高佳维[1] 顾炜东 岳铫辰 周旭 闫丽梅 范开[1] Wang Yuqi;He Fei;Wei Yong;Rong Zhaojin;Gao Jiawei;Gu Weidong;Yue Yaochen;Zhou Xu;Yan Limei;Fan Kai(Key Laboratory of Earth and Planetary Physics,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,Beijing 100049,China)

机构地区：[1]中国科学院地质与地球物理研究所地球与行星物理重点实验室,北京100029 [2]中国科学院大学地球与行星科学学院,北京100049

出　　处：《地球与行星物理论评（中英文）》2024年第6期705-718,共14页Reviews of Geophysics and Planetary Physics

基　　金：中国科学院青年交叉团队资助项目(JCTD-2021-05)。

摘　　要：地磁场与气候相关性研究五十年,人们并没有完全理解地磁场变化如何调控气候,反而更深刻地意识到这个问题远比之前想象的要复杂.本文从不同的时空尺度梳理了过去五十年间对于地磁场与气候关联性的研究.研究表明,从万年尺度的地磁倒转、千年尺度的地磁漂移、到百年尺度的考古地磁急变,甚至年代际的地磁活动变化,各种尺度的地磁场变化与气候之间都存在显著的关联.然而,相关性并不代表因果性,地磁场影响气候变化的潜在机制仍然存在争论.宇宙射线生成云机制是目前最有潜力的地磁场调控气候的过程,它在不同的时间尺度上有效地发挥作用,但其确切的物理机制和相对重要性仍然是悬而未决的问题.本文提议,应当从日地多圈层耦合的角度去理解地磁场与气候的关联性,并重点关注区域气候系统对区域磁场变化的响应.从古到今、从点到面,最终形成关联地磁场与气候变化的全球图像.如今,可精细刻画南大西洋异常区(SAA)磁场变化的澳科一号的成功发射,百年尺度的西太平洋磁异常区(WPA)的首次发现以及古地磁/考古地磁和古气候数据重构的快速发展为地磁场与气候研究提供了新的历史机遇,地磁场变化对气候的影响研究将被推向新的高潮.After 50 years of research on the correlation between the geomagnetic field and climate,we have gained a deeper understanding that the regulation of climate by geomagnetic field changes is far more complex than previously imagined.In this paper,we comprehensively review the research connecting the geomagnetic field and climate over the past 50 years,examining different spatial and temporal scales.Our results demonstrate a significant correlation between geomagnetic field changes and climate at various scales,including millennial-scale geomagnetic reversals,thousand-year-scale geomagnetic shifts,centennial-scale geomagnetic abrupt,and even decadalscale variations in geomagnetic activity.The Matuyama–Brunhes geomagnetic reversal is associated with the cold climate.The increase in galactic cosmic rays(GCR)during this period gave rise to the formation of low-altitude cloud"umbrella effects",subsequently weakening the East Asian summer monsoon and intensifying the East Asian winter monsoon.Archaeomagnetic data from Mesopotamia remarkably illustrates a consistent correlation between four cold periods in the last three thousand years and a sudden increase in geomagnetic anomalies.Exploring the possibility that these geomagnetic anomalies correspond to extreme tilts of the Earth's dipole,it is hypothesized that auroral ovals and sub-auroral regions may have expanded to lower latitudes.In these regions,cosmic rays poten-tially interacted with a more humid troposphere,resulting in increased cloud cover and,consequently,observed at-mospheric cooling.Changes in GCR flux,induced by solar activity and variations in the geomagnetic field,are pro-posed to have significant implications for alterations in temperate pressure systems,precipitation patterns,and at-mospheric electric fields.These effects play diverse roles within the intricately coupled system of the Earth's atmo-sphere and the near-Earth space environment.However,it's important to note that correlation does not imply causa-tion,and the potential mechanisms by which

关 键 词：地磁场 气候 宇宙射线 日地系统 

分 类 号：P318[天文地球—固体地球物理学]