利用COSMIC-1/2 IonPrf产品分析中国区域近15年电离层时空变化特征

Analysis of Temporal-Spatial Variation Characteristics of Ionosphere over China Region in the Past 15 Years Using COSMIC-1/2 IonPrf Products

  • 摘要: 利用2006—2020年中国区域的COSMIC-1/2 (constellation observing system for meteorology ionosphere and climate-1/2) IonPrf产品数据,分析了中国区域电离层时空变化特征。首先介绍新一代COSMIC-2在中国以及全球区域的数据质量状况;然后对IonPrf产品的数据质量控制和电离层特征参数提取方法进行说明;最后,以不同时间尺度统计分析了中国区域近15年电离层特征参数在一个完整太阳活动周期不同活动水平下的时空变化特征。统计结果表明,中国区域电离层变化具有与太阳活动相关的周年变化、季节变化和日变化特征;周年变化中具有明显空间分布特征,以30°N左右为界,中国南方地区峰值密度NmF2、峰值高度HmF2和电子总含量(total electron content,TEC)年均值普遍高于北方地区;在月份季节变化中,NmF2和TEC最大值一般出现在3月、10月,最小值出现在6月、7月,仅中国南方部分地区存在冬季异常现象,且春、夏季的HmF2均值大于秋、冬季;在日变化中,NmF2和TEC的最大值主要出现在地方时(local time,LT)12:00—16:00,且峰值对应的地方时随纬度升高而向前推移。当太阳活动高年时,日落后NmF2和TEC仍保持较高水平。HmF2在中国南方地区最大值出现在LT 12:00—16:00,最小值出现在LT 05:00—07:00,北方地区HmF2的值白天普遍低于夜间。

     

    Abstract:
    Objectives Using IonPrf of COSMIC (constellation observation system for meteorology ionosphere and climate) measurements during 2006—2020, the temporal-spatial variation characteristics of ionosphere is analyzed over China region.
    Methods First, the quality of new generation COSMIC-2 data is introduced over China and global regions. Then, the method of extracting the ionospheric characteristic parameters and controlling the quality of IonPrf products data is illustrated. Finally, the temporal-spatial variation characteristic of ionospheric parameters is analyzed over China region for 15 years during a complete solar cycle by different time scale.
    Results Experimental results show that the ionospheric variation of China region has the characteristic of annual, seasonal, and diurnal variation related to solar activity. In annual variation, NmF2, HmF2 and total electron content(TEC) in southern China being generally higher than those in northern China, has obvious spatial distribution characteristic. In seasonal variation, NmF2 and TEC have maximum in March and October, and minimum in June and July.
    Conclusions The winter anomaly only appears in parts of southern China and the average of HmF2 in spring and autumn is higher than one in summer and winter. In diurnal variation, NmF2 and TEC have maximum during local time 12:00-16:00 and the local time corresponding to the peak value moves forward with increasing of latitude. The NmF2 and TEC are still high relatively after sunset during year of solar high activity. HmF2 of southern China has maximum during local time 12:00-16:00 and minimum during local time 05:00—07:00. And HmF2 of northern China in daytime is generally lower than one in night.

     

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