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21.
本文简要介绍了相干散射雷达SABRE及其观测Pc5地磁脉动的工作原理。1985—1989年观测数据的统计分析结果表明,相位向极传播脉动事件的出现率峰值在当地时间午夜附近,而向赤道传播事件的出现率峰值则在18:00LT左右。文中给出了上述两类脉动事件出现率的日变化,与地磁活动的相关,与背景电离层等离子体对流特性的关系等统计分析结果。 相似文献
22.
广州地磁Z分量日变幅的谱特征 总被引:1,自引:0,他引:1
利用1972—1993年广州地磁资料,分析了Z分量日变幅的年平均、年变化和半年变化等低频成分的逐年变化,以及小于60天的短周期变化特征.同时对1972—1993年的F10.7日均值进行了谱分析.结果指出,广州地磁Z分量日变幅的年平均与太阳活动指数F10.7的年平均存在良好的线性相关;具有幅度大约5nT夏季极大的年变化,与太阳活动没有明显相关,是一种季节效应;存在春秋分极大的半年变化,幅度与太阳活动有关,高年的幅度明显大于低年;具有明显的与太阳自转相关的27天左右的变化和明显的与行星波有关的接近16日、10日、5日、2日等短周期变化.广州地磁Z分量日变幅的这些谱特征,有助于更深入地了解中低层大气对电离层影响的物理机制. 相似文献
23.
This paper analyzes the state of the ionosphere during two geomagnetic storms of a different intensity evolving in different sectors of local time in different seasons. There were used the data from a network of ionospheric stations located in the opposite longitudinal sectors of 80°-150° E and 250°-310° E.This analysis has permitted us to conclude that the detected differences in the variations of the disturbances are likely to be determined by the local time difference of the geomagnetic storm development, its intensity and by the different illumination conditions of the ionosphere. 相似文献
24.
QIN Guotai QIU Shiyan HE Aiqing Zhu Yiqiang SUN Lilin LIN Xianwen LI Hong XU Xuepei 《空间科学学报》2002,22(Z1)
Upper atmosphere composition data were obtained for the last half year with a quadruple mass spectrometer on board spacecraft "SZ-2" launched on 10 Jan uary 2001. Based on the analysis of these data, the variations of atmospheric compositions in solar and geomagnetic quiet conditions are reported first, then a detailed discussion on the atmospheric composition variations under the so lar and geomagnetic disturbed conditions is given. The results show that near the altitude of 400 km the variations of main atmospheric compositions corre sponding to solar disturbances are more remarkable in the sunlit area than in the shade area. On the contrary, in geomagnetic disturbance events the corre sponding variations are more obvious in the shade area, an evident increase of N2 density at relatively higher latitudes was observed. 相似文献
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用Morlet小波变换对Oulu台站和Apatity台站(主要是Apatity台站)1998-2002年间宇宙线静日和地磁暴前的地面宇宙线强度变化特征进行分析,得到:在宇宙线静日期间普遍存在准24h周期变化特征,并且在当地时间0200,1400左右分别出现最小值和最大值;对12个例子的分析可以看到地面宇宙线强度在地磁暴之前l-2天均出现了不同于宇宙线静日期间变化特征,或有小尺度周期出现,或周期变化完全消失,或有异常24h周期变化,这种变化特征在一定程度上可作为地磁预报的先兆特征之一。 相似文献
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Alicia L. Clúa de Gonzalez Walter D. Gonzalez 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2013
In the present paper the local-time variations in the disturbance of the geomagnetic-field horizontal component (H) for eight intense geomagnetic storms that occurred during the descending phase of solar cycle 23 have been analyzed. The study was based on the plot of contour lines of the H-depletion intensity in the plane local time versus universal time (LT–UT maps) with the objective of observing how the morphology and evolution of the ring current is mapped into the surface of the Earth in presence of intense geomagnetic storms. 相似文献
29.
利用EISCAT雷达探测数据,分析计算了太阳活动高年夏季发生的一次强磁暴期间,极光区电离层对流电场、电导率以及焦耳加热速率等着重考察了E区热怪大气焦耳加热和F区离子摩擦增温与F区电子密度耗空的关系发现在下午东向极光电集流期间,电子密度最大耗空出现在F区300-325km高度,时间恰在积分的E区大气焦耳加热量大值和F区最大离子增温之后5-10min,耗空率达70%。 相似文献
30.
Gustavo A. Mansilla 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2011
This paper reports the global response of the mid high and low latitude ionosphere in four longitudinal sectors to two moderate geomagnetic storms that occurred during 2007 (the more intense storms occurred that year). The results obtained during these storms show that the ionospheric effects in general are not moderate in magnitude, showing an important degree of complexity as during intense storms. The outstanding features produced during the storms are significant positive storm effects at mid-high latitudes during the main phase/first part of the recovery, positive effects after the onset of the storm followed by negatives effects at middle latitudes and delayed positive effects during the night-time hours in the trough of the equatorial anomaly (“dusk” effect). Possible physical mechanisms for controlling the morphology of the ionosphere during these events are considered. 相似文献