IONOSPHERIC CURRENT STRUCTURE AS DETERMINED FROM GROUND-BASED MAGNETOMETER DATA

被引:20
作者
OLDENBURG, DW [1 ]
机构
[1] UNIV ALBERTA, INST EARTH & PLANETARY PHYS, DEPT PHYS, EDMONTON T6G 2E1, ALBERTA, CANADA
来源
GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY | 1976年 / 46卷 / 01期
关键词
D O I
10.1111/j.1365-246X.1976.tb01631.x
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
引用
收藏
页码:41 / 66
页数:26
相关论文
共 12 条
[2]   UNIQUENESS IN INVERSION OF INACCURATE GROSS EARTH DATA [J].
BACKUS, G ;
GILBERT, F .
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY OF LONDON SERIES A-MATHEMATICAL AND PHYSICAL SCIENCES, 1970, 266 (1173) :123-&
[3]  
BERKTOLD A, 1974, 2ND WORKSH EL IND EA
[4]  
Birkeland K., 1908, NORWEGIAN AURORA POL, V1
[5]   A 3-DIMENSIONAL MODEL CURRENT SYSTEM FOR POLAR MAGNETIC SUBSTORMS [J].
BONNEVIER, B ;
BOSTROM, R ;
ROSTOKER, G .
JOURNAL OF GEOPHYSICAL RESEARCH, 1970, 75 (01) :107-+
[6]   PARTIAL RING CURRENT MODELS FOR WORLDWIDE GEOMAGNETIC DISTURBANCES [J].
FUKUSHIMA, N ;
KAMIDE, Y .
REVIEWS OF GEOPHYSICS, 1973, 11 (04) :795-853
[7]  
GILBERT F, 1971, GEOPHYS J ROY ASTR S, V23, P125, DOI 10.1111/j.1365-246X.1971.tb01807.x
[8]  
KISABETH JL, 1972, THESIS U ALBERTA
[9]   PHASE RELATIONS BETWEEN POLAR MAGNETIC SUBSTORM FIELDS AT SURFACE OF A FINITELY CONDUCTING EARTH [J].
NOPPER, RW ;
HERMANCE, JF .
JOURNAL OF GEOPHYSICAL RESEARCH, 1974, 79 (31) :4799-4801
[10]  
ONWUMECHILLI A, 1967, J ATMOS TERR PHYS, V29, P533