摘要
本文利用1991年度南极中山站的地磁资料,分析研究极夜(5、6、7月)及极昼(11、12月)期间S、SD的变化特征。研究结果表明,H、D、Z三个分量的S、SD在极夜期间的变化幅度都小于极昼期间的变化幅度,S在世界时UT6时左右出现极值。这是由于在5、6、7月的太阳直射点在北半球,太阳紫外辐射和X射线辐射减少,在11、12月太阳的直射点在南半球,太阳紫外线和X射线辐射增大,致使空间电高层等效电流发生变化所产生。
The variation regularity and the Characteristics of S,SD during the polar day (Nov. and Dec.)and the polar night (May.,June., July.) are analyzed and investigated here using the geomagnetic data from Zhongshang Station Antarctica in 1991. The results show that the variation amplitudes of S,SD of the three components,H,D and Z, during the polar night are smaller than those during the polar day. Because the solar purple rays and X-rays radiation decrease in Antarctica in May., June. and July., due to that the sunlight directly radiates at the Northern hemisphere during that time; but in Nov, and Dec.,so that the currents in the ionosphere vary.
出处
《地震地磁观测与研究》
1996年第2期50-56,共7页
Seismological and Geomagnetic Observation and Research
关键词
地磁场
南极
中山站
极夜
极昼
变化规律
geomagnetic field, Zhongshang Antarctica Station,polar night,polar day