Secular variations in geomagnetic field caused by the fluctuations in the fluid flow in the outer-core

被引:3
|
作者
Liu, QS [1 ]
Zhu, RX [1 ]
Pan, YX [1 ]
Guo, B [1 ]
机构
[1] Chinese Acad Sci, Inst Geophys, Beijing 100101, Peoples R China
来源
CHINESE SCIENCE BULLETIN | 1999年 / 44卷 / 13期
基金
中国国家自然科学基金;
关键词
r(0); geomagnetic Jerk; length-of-day;
D O I
10.1007/BF02885969
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The theoretical spatial power spectrum of a dipole located at ( r(0), theta(0), phi(0)) can be fitted by a straight line in logarithmic scale when n is larger than 2. Based on the spherical harmonic coefficients of geomagnetic field during 1900-1995, the depth( r(0)) of source-layer of every 5a is calculated. The results show that r(0) decreased from 1900 to 1960; abruptly changed from 1945 to 1950 related to some kind of disturbance; decreased again from 1960 to 1975; increased from 1975 to 1985; and kept stable after 1985. Then the mean energy density (MED) of each year is Induced to ifs corresponding r(0). We find that MED of dipole field kept nearly unchanged from 1900 to 1960. While, MED of non-dipole field increased. The change of r(0) coinciding with the geomagnetic secular variation, impulse and length-of-day happened around 1970, suggesting that the change of r(0) may be related to the impulse. The variation in the fluid flow in the outer-core caused by the core-mantle coupling is a plausible candidate in explaining the changes in geomagnetic Jerk, length-of-day, and r(0).
引用
收藏
页码:1214 / 1218
页数:5
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