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首页> 外文期刊>Geomagnetism and aeronomy >Diurnal Variations in the Statistical Characteristics of the Variability of the Midlatitude NmF2 during Quiet Geomagnetic Conditions at Low Solar Activity
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Diurnal Variations in the Statistical Characteristics of the Variability of the Midlatitude NmF2 during Quiet Geomagnetic Conditions at Low Solar Activity

机译:低太阳能活动期间,在静音地磁条件下,中位数NMF2变异性的差变化

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摘要

The work examines diurnal variations in the statistical characteristics of the variability of the electron number density NmF2 of the maximum of the ionspheric F2 layer during quiet geomagnetic conditions at low solar activity based on hourly ionosonde measurements of the critical frequency of the ionspheric F2 layer from 1957 to 2017 over Moscow. The statistical parameters of NmF2 are calculated for each month M of each year at the universal time UT = 0, 1, horizontal ellipsis 23 h: the mathematical expectation NmF2(E); the most probable value NmF2(MP); the average monthly median NmF2(MED); the arithmetic mean NmF2(A); the standard deviations of NmF2 from NmF2(E), NmF2(MP), and NmF2(MED); and the coefficients of variation CVE, CVMP, and CVMED of NmF2 relative to NmF2(E), NmF2(MP), and NmF2(MED), respectively. It follows from the calculations that the CVE, CVMED, and CVMP values vary within the intervals of 12-43%, 12-60%, and 13-75%, respectively, and, in the vast majority of cases, CVE(UT, M) < CVMED(UT, M) and CVE(UT, M) < CVMP(UT, M). If the coefficient CVE in each month of each year is compared for different time points, the lowest CVE value varies from 12% (July) to 19% (December) and occurs during daytime, while the highest CVE value lies in the interval from 26% (June) to 43% (December). For each UT, the lowest and highest values of this coefficient in the autumn, winter, and spring months are greater than those for the summer months. It was found that the difference of NmF2(A)(UT, M) from NmF2(E)(UT, M) does not exceed 0.2%.
机译:该作品在低太阳能活动期间,基于1957年的临界频率测量的低太阳能活动期间,在低太阳能活动期间,在低太阳能活性期间,在低太阳能活动期间,在低太阳能活动期间,对电子数密度NMF2的变化的统计特征的统计特征的统计特征差异。到2017年莫斯科。 NMF2的统计参数计算每年的每个月M在通用时间UT = 0,1,水平椭圆23小时:数学期望NMF2(E);最可能的价值NMF2(MP);平均月中位数NMF2(MED);算术平均nmf2(a); NMF2来自NMF2(E),NMF2(MP)和NMF2(MED)的标准偏差;分别的变异系数CVE,CVMP和NMF2的CVME,CVMP和CVMED分别相对于NMF2(e),NMF2(MP)和NMF2(MED)。它从CVE,CVMED和CVMP值分别在12-43%,12-60%和13-75%之间变化,并且在绝大多数情况下,CVE(UT, m)

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  • 来源
    《Geomagnetism and aeronomy》 |2019年第5期|共13页
  • 作者

    Pavlov A. V; Pavlova N. M.;

  • 作者单位

    Russian Acad Sci Pushkov Inst Terr Magnetism Ionosphere &

    Radio Wa Moscow Russia;

    Russian Acad Sci Pushkov Inst Terr Magnetism Ionosphere &

    Radio Wa Moscow Russia;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;
  • 关键词

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