中国区域地磁场垂直分量日变化特征分析与研究

张秀玲, 赵旭东, 范晓勇

张秀玲,赵旭东,范晓勇. 2024. 中国区域地磁场垂直分量日变化特征分析与研究. 地震学报,46(6):1014−1023. DOI: 10.11939/jass.20230065
引用本文: 张秀玲,赵旭东,范晓勇. 2024. 中国区域地磁场垂直分量日变化特征分析与研究. 地震学报,46(6):1014−1023. DOI: 10.11939/jass.20230065
Zhang X L,Zhao X D,Fan X Y. 2024. Research on daily variation of vertical component of geomagnetic field in China. Acta Seismologica Sinica46(6):1014−1023. DOI: 10.11939/jass.20230065
Citation: Zhang X L,Zhao X D,Fan X Y. 2024. Research on daily variation of vertical component of geomagnetic field in China. Acta Seismologica Sinica46(6):1014−1023. DOI: 10.11939/jass.20230065

中国区域地磁场垂直分量日变化特征分析与研究

基金项目: 中国地震局地球物理研究所基本科研业务费专项(DQJB23Z02)资助
详细信息
    作者简介:

    张秀玲,高级工程师,现从事地震监测工作,e-mail:505234577@qq.com

  • 中图分类号: P318.1

Research on daily variation of vertical component of geomagnetic field in China

  • 摘要:

    基于我国地磁台站的观测数据,首先根据地磁台垂直分量日变化曲线的形态特征,统计了15个地磁台站垂直分量的极小时间(地方时),并重点探讨了这些极小时间在我国区域内的分布特性及其与台站经度的关系。其次选取27个地磁台垂直分量太阳活动高年与太阳活动低年年均值日变幅,分析垂直分量日变幅与太阳黑子活动之间的关系,并按照劳埃德季节划分的分点月份,夏至点月份、冬至点月份等不同季节及太阳活动高低年分别探讨垂直分量日变幅在不同季节和太阳活动高低年的变化规律及特性。研究结果表明:① 我国区域内地磁场垂直分量的极小时间主要集中在当地正午附近,与台站的经度呈显著负相关关系,并且该时间分布符合正态分布模式;② 地磁场垂直分量的日变幅显著受太阳黑子活动的影响,与太阳黑子数的相关系数为0.929,二者存在高度正相关性,垂直分量的日变幅显示出约11年的周期性变化;③ 垂直分量的日变幅变化受季节影响,表现出明显的季节性差异,地磁场日变幅在夏至点月份比冬至点月份更为活跃,在不同季节产生不同影响。研究结果为了解地磁场日变化特征和规律及地球内部活动提供了依据和参考。

    Abstract:

    Based on the observation data from geomagnetic stations in China, we first statistically analyzed the minimum time (local time) of the vertical component at 15 geomagnetic stations based on its morphological characteristics of the daily variation curves. We then focused on the distribution characteristics of these minimum times within the Chinese region and their relationship with the longitude of the stations. Secondly, we selected 27 geomagnetic stations to analyze the annual average daily variation amplitudes of the vertical component during periods of high and low solar activity, aiming to achieve the relationship between the daily variation amplitudes of the vertical component and sunspot activity. This analysis was conducted for different seasons, including the months around the equinoxes, summer solstice, and winter solstice, as well as for years with high and low solar activity. The results show that: ① The minimum time of the vertical component of the geomagnetic field in China is mainly concentrated around local noon, showing a significant negative correlation with the longitude of the stations, and this time distribution follows a normal distribution pattern. ② The daily variation amplitude of the vertical component of the geomagnetic field is significantly influenced by sunspot activity, by a correlation coefficient of 0.929 with the number of sunspots, indicating a strong positive correlation. The daily variation amplitude of the vertical component exhibits a cyclic change of about 11 years. ③ The daily variation amplitude of the vertical component shows seasonal differences, being more active in the months around the summer solstice compared to the months around the winter solstice, indicating distinct seasonal impacts. These findings provide insights into the daily variation characteristics and patterns of the geomagnetic field and offer references for understanding Earth's internal activities.

  • 图  1   我国地磁台分布示意图

    Figure  1.   Map of geomagnetic station distribution in China

    图  2   2014年1月16日红山地磁台(LYH)垂直分量Z日变化曲线图

    Figure  2.   Daily variation curve of the vertical component at Hongshan geomagnetic station on January 16th,2014

    图  3   垂直分量Z极小值时间分布图

    Figure  3.   Minimum time distribution of vertical component Z

    图  4   2000—2020年地磁场垂直分量日变幅ΔZ(黑色)与太阳黑子数R(红色)曲线对比图

    Figure  4.   Comparison of daily variation amplitude of vertical component of geomagnetic field (ΔZ) curves (black) and sunspot number R (red) curves during 2000−2020

    图  5   2014年(太阳活动高年)和2019年(太阳活动低年)地磁场垂直分量日变幅差值图

    Figure  5.   Daily variation amplitude difference between 2014 (solar maximum) and 2019 (solar minumum)

    图  6   地磁场垂直分量在太阳活动高年(2014年)(左)和太阳活动低年(2019年)(右)不同季节的日变幅等值线图

    (a) 分点月份;(b) 夏至点月份;(c) 冬至点月份

    Figure  6.   Contour map of daily variation amplitude of vertical component in geomagnetic field in different seasons in high solar year (2014)(left) and low solar year (2019) (right)

    (a) Equinox month;(b) Summer solstice month;(c) Winter solstice month

    图  7   太阳活动高年(2014)(a)和太阳活动低年(2019)(b)地磁场垂直分量日变幅等值线图

    Figure  7.   Contour map of daily variation amplitude of vertical component in geomagnetic field in high (2014) and low (2019) solar activity years

    表  1   2014年我国Z分量极小值时间统计表

    Table  1   The minimum time statistics of Z-component in China in 2014

    序号台站名简称极小值时间序号台站名简称极小值时间
    1喀 什KSH14:139太 原TAY12:36
    2乌鲁木齐WMQ13:5810红 山LYH12:25
    3拉 萨LSA13:4611静 海JIH12:19
    4格尔木GLM13:4112满洲里MZL11:51
    5西 昌XIC12:5813大 连DLG11:50
    6通 海THJ12:5814长 春CHC11:42
    7成 都CDP12:5815德 都DED11:10
    8邕 宁YON12:40
    下载: 导出CSV

    表  2   2000—2020年地磁场垂直分量日变幅与太阳黑子数量间的相关系数

    Table  2   Correlation coefficients between daily variation amplitude and sunspot number during 2000−2020

    地磁台站 相关系数 地磁台站 相关系数
    CHC 0.932 LZH 0.843
    COM 0.925 THJ 0.855
    CDP 0.987 WLM 0.937
    LSA 0.968 QGZ 0.912
    LYH 0.977
    下载: 导出CSV
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出版历程
  • 收稿日期:  2023-05-31
  • 修回日期:  2023-09-25
  • 录用日期:  2023-10-06
  • 网络出版日期:  2024-12-17
  • 刊出日期:  2024-11-19

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